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rupture"},{"average_dip":"(90,,)","average_rake":"(0,,)","catalog_id":"NEA_6","catalog_name":"GEM_NE_Asia","name":"Erzin-Agar-Dag Fault","slip_type":"Sinistral","reference":"DEM; Arzannikov and Arzannikova 2009","epistemic_quality":"1","accuracy":"85000","activity_confidence":"1","exposure_quality":"2","notes":"Little geomorphic expression of this section of the fault trace"},{"average_dip":"(70,45,90)","average_rake":"(22.5,0,67.5)","catalog_id":"NEA_7","catalog_name":"GEM_NE_Asia","dip_dir":"N","name":"Erzin-Agar-Dag Fault","slip_type":"Sinistral-Reverse","reference":"DEM; Arzhannikov and Arzhannikova, 2009","epistemic_quality":"1","accuracy":"60000","activity_confidence":"1","downthrown_side_dir":"S","exposure_quality":"1"},{"average_dip":"(90,,)","average_rake":"(0,,)","catalog_id":"NEA_8","catalog_name":"GEM_NE_Asia","name":"Erzin-Agar-Dag Fault","slip_type":"Sinistral","reference":"DEM; Arzhannikov and Arzhannikova, 2009","epistemic_quality":"1","accuracy":"80000","activity_confidence":"1","exposure_quality":"1"},{"average_dip":"(70,50,90)","average_rake":"(22.5,0,45.)","catalog_id":"NEA_9","catalog_name":"GEM_NE_Asia","dip_dir":"N","name":"Erzin-Agar-Dag Fault","slip_type":"Sinistral-Reverse","reference":"DEM; Arzhannikov and Arzhannikova, 2009","epistemic_quality":"1","accuracy":"50000","activity_confidence":"1","downthrown_side_dir":"S","exposure_quality":"1"},{"average_dip":"(90,,)","catalog_id":"NEA_10","catalog_name":"GEM_NE_Asia","name":"Erzin-Agar-Dag Fault","slip_type":"Sinistral","reference":"DEM","epistemic_quality":"1","accuracy":"90000","activity_confidence":"1","exposure_quality":"2"},{"average_dip":"(90,,)","catalog_id":"NEA_11","catalog_name":"GEM_NE_Asia","name":"Mayna Fault","slip_type":"Sinistral","reference":"DEM","epistemic_quality":"1","accuracy":"70000","activity_confidence":"2","exposure_quality":"2","notes":"Found on DEM, can't find much reference."},{"average_dip":"(90,,)","catalog_id":"NEA_12","catalog_name":"GEM_NE_Asia","name":"Mayna Fault","slip_type":"Sinistral","reference":"DEM","epistemic_quality":"1","accuracy":"100000","activity_confidence":"2","exposure_quality":"2","notes":"Big fault, maybe active. Some geomorphic expression in older Quaternary seds but nothing great."},{"average_dip":"(90,,)","catalog_id":"NEA_13","catalog_name":"GEM_NE_Asia","name":"Mayna Fault","slip_type":"Sinistral","reference":"DEM","epistemic_quality":"2","accuracy":"70000","activity_confidence":"2","exposure_quality":"2"},{"average_dip":"(90,,)","catalog_id":"NEA_14","catalog_name":"GEM_NE_Asia","name":"Har-Us-Nuur Fault","slip_type":"Dextral","reference":"DEM, ...","epistemic_quality":"1","accuracy":"70000","activity_confidence":"1","exposure_quality":"2"},{"average_dip":"(90,,)","catalog_id":"NEA_15","catalog_name":"GEM_NE_Asia","name":"Har-Us-Nuur Fault","slip_type":"Dextral","reference":"DEM, ...","epistemic_quality":"1","accuracy":"70000","activity_confidence":"1","exposure_quality":"2"},{"average_dip":"(90,,)","catalog_id":"NEA_16","catalog_name":"GEM_NE_Asia","name":"Har-Us-Nuur Fault","slip_type":"Dextral","reference":"DEM; Gregory et al., 2014","epistemic_quality":"1","accuracy":"60000","activity_confidence":"1","strike_slip_rate":"(2.4,2.0,2.8)","exposure_quality":"1","notes":"Slip rate from Gregory"},{"average_dip":"(90,,)","catalog_id":"NEA_17","catalog_name":"GEM_NE_Asia","name":"Har-Us-Nuur Fault","slip_type":"Dextral","reference":"DEM; Gregory et al., 2014","epistemic_quality":"1","accuracy":"60000","activity_confidence":"1","strike_slip_rate":"(2.4,2.0,2.8)","exposure_quality":"1","notes":"Slip rate from Gregory"},{"average_dip":"(90,,)","catalog_id":"NEA_18","catalog_name":"GEM_NE_Asia","name":"Har-Us-Nuur Fault","slip_type":"Dextral","reference":"DEM","epistemic_quality":"1","accuracy":"60000","activity_confidence":"1","exposure_quality":"1"},{"average_dip":"(90,,)","catalog_id":"NEA_19","catalog_name":"GEM_NE_Asia","dip_dir":"N","slip_type":"Sinistral","reference":"DEM, Google Earth","epistemic_quality":"1","accuracy":"60000","activity_confidence":"1","downthrown_side_dir":"S","exposure_quality":"1"},{"average_dip":"(90,,)","catalog_id":"NEA_20","catalog_name":"GEM_NE_Asia","name":"Kubadru Fault","slip_type":"Dextral","reference":"DEM; Deev et al. 2017","epistemic_quality":"1","accuracy":"150000","activity_confidence":"1","exposure_quality":"1"},{"average_dip":"(90,,)","catalog_id":"NEA_21","catalog_name":"GEM_NE_Asia","name":"Chuya Fault","slip_type":"Dextral","reference":"Dorthbath et al., 2008 BSSA; Nissen et al. 2007","epistemic_quality":"1","accuracy":"300000","activity_confidence":"1","last_movement":"2003","exposure_quality":"1","notes":"Ruptured in the 2003 Gorny Altay EQ (Mw 7.2). Fault trace is more or less impossible to see in DEM."},{"average_dip":"(50,30,70)","average_rake":"(67.5,45,90)","catalog_id":"NEA_22","catalog_name":"GEM_NE_Asia","dip_dir":"N","name":"Uureg Nuur Fault","slip_type":"Reverse-Sinistral","reference":"DEM; Walker et al 2006","epistemic_quality":"1","accuracy":"60000","activity_confidence":"1","last_movement":"1970","downthrown_side_dir":"S","exposure_quality":"2"},{"average_dip":"(90,,)","average_rake":"(90,,)","catalog_id":"NEA_23","catalog_name":"GEM_NE_Asia","name":"Hovd Fault (Chihteyn Segment)","slip_type":"Dextral","reference":"Khil'ko et al., 1985; Baljinnyam et al. 1993","epistemic_quality":"1","accuracy":"50000","activity_confidence":"1","strike_slip_rate":"(0.5,,)","exposure_quality":"1"},{"average_dip":"(90,,)","catalog_id":"NEA_24","catalog_name":"GEM_NE_Asia","name":"Hovd Fault (north-central segment)","net_slip_rate":"(0.5,,)","slip_type":"Dextral","reference":"Slip rate quoted in Frankel et al., 2010; original source uncertain","epistemic_quality":"1","accuracy":"60000","activity_confidence":"1","exposure_quality":"1"},{"average_dip":"(90,,)","catalog_id":"NEA_25","catalog_name":"GEM_NE_Asia","name":"Hovd Fault (Ar Hotol segment)","net_slip_rate":"(1.2,,)","slip_type":"Dextral","reference":"DEM, Google Earth","epistemic_quality":"1","accuracy":"50000","activity_confidence":"1","fs_name":"Hovd Fault","exposure_quality":"1","notes":"Slip rate listed in Frankel et al. 2010; source uncertain"},{"average_dip":"(20,15,30)","average_rake":"(90,,)","catalog_id":"NEA_26","catalog_name":"GEM_NE_Asia","dip_dir":"N","name":"Kurai Fault","slip_type":"Reverse","reference":"DEM; Deev et al., 2017","epistemic_quality":"1","accuracy":"90000","activity_confidence":"1","downthrown_side_dir":"S","exposure_quality":"2"},{"average_dip":"(20,15,30)","average_rake":"(90,,)","catalog_id":"NEA_27","catalog_name":"GEM_NE_Asia","dip_dir":"N","name":"Kurai Thrust","slip_type":"Reverse","reference":"DEM; Deev et al., 2017","epistemic_quality":"1","accuracy":"70000","activity_confidence":"1","downthrown_side_dir":"S","exposure_quality":"2"},{"average_dip":"(20,15,30)","average_rake":"(90,,)","catalog_id":"NEA_28","catalog_name":"GEM_NE_Asia","dip_dir":"N","name":"Kurai Fault","slip_type":"Reverse","reference":"DEM; Deev et al. 2017","epistemic_quality":"1","accuracy":"70000","activity_confidence":"1","downthrown_side_dir":"S","exposure_quality":"1"},{"average_dip":"(25,15,30)","average_rake":"(90,,)","catalog_id":"NEA_29","catalog_name":"GEM_NE_Asia","dip_dir":"N","name":"Kurai Fault","slip_type":"Reverse","reference":"DEM; Deev et al., 2017","epistemic_quality":"1","accuracy":"90000","activity_confidence":"1","downthrown_side_dir":"S","exposure_quality":"1"},{"average_dip":"(50,30,70)","average_rake":"(67.5,45,90)","catalog_id":"NEA_84","catalog_name":"GEM_NE_Asia","dip_dir":"N","name":"Uureg Nuur Fault (west)","slip_type":"Reverse-Sinistral","reference":"DEM; Tapponnier and Molnar, 1979; Vilkas 1982; Khil'ko 1985","epistemic_quality":"1","accuracy":"50000","activity_confidence":"1","last_movement":"1970","downthrown_side_dir":"S","exposure_quality":"1","notes":"Looks pretty reverse, but some left-lateral slip apparent in (poorly-constained?) focal mechanism, and field observations by Khil'ko"},{"average_dip":"(25,20,45)","average_rake":"(90,,)","catalog_id":"NEA_31","catalog_name":"GEM_NE_Asia","dip_dir":"S","slip_type":"Reverse","reference":"DEM; Walker et al., 2006","epistemic_quality":"2","accuracy":"90000","activity_confidence":"2","downthrown_side_dir":"N","exposure_quality":"2"},{"average_dip":"(90,60,90)","average_rake":"(180,135,180)","catalog_id":"NEA_32","catalog_name":"GEM_NE_Asia","dip_dir":"W","slip_type":"Dextral","reference":"DEM; Walker et al., 2006","epistemic_quality":"2","accuracy":"90000","activity_confidence":"2","downthrown_side_dir":"E","exposure_quality":"2","notes":"Possible reverse component given structural and topographic context"},{"average_dip":"(20,15,30)","average_rake":"(90,,)","catalog_id":"NEA_33","catalog_name":"GEM_NE_Asia","dip_dir":"S","slip_type":"Reverse","reference":"DEM","epistemic_quality":"1","accuracy":"50000","activity_confidence":"1","downthrown_side_dir":"N","exposure_quality":"1"},{"average_dip":"(30,20,50)","average_rake":"(180,112.5,180)","catalog_id":"NEA_34","catalog_name":"GEM_NE_Asia","dip_dir":"E","slip_type":"Reverse","reference":"DEM; Walker et al. 2006","epistemic_quality":"1","accuracy":"50000","activity_confidence":"1","downthrown_side_dir":"W","exposure_quality":"1","notes":"Walker notes possible dextral component, especially in north"},{"average_dip":"(25,15,35)","average_rake":"(90,,)","catalog_id":"NEA_35","catalog_name":"GEM_NE_Asia","dip_dir":"E","slip_type":"Reverse","reference":"Walker et al 2006","epistemic_quality":"1","accuracy":"70000","activity_confidence":"1","downthrown_side_dir":"W","exposure_quality":"1"},{"average_dip":"(25,15,35)","average_rake":"(90,,)","catalog_id":"NEA_36","catalog_name":"GEM_NE_Asia","dip_dir":"W","slip_type":"Reverse","reference":"DEM; Walker et al. 2006","epistemic_quality":"1","accuracy":"50000","activity_confidence":"1","downthrown_side_dir":"E","exposure_quality":"1"},{"average_dip":"(50,30,65)","average_rake":"(90,90,135)","catalog_id":"NEA_37","catalog_name":"GEM_NE_Asia","dip_dir":"E","slip_type":"Reverse","reference":"DEM; Nissen et al. 2009","epistemic_quality":"1","accuracy":"90000","activity_confidence":"1","downthrown_side_dir":"W","exposure_quality":"1","notes":"Possible dextral component; surely merges with Haar us Nuur fault at depth"},{"average_dip":"(90,,)","catalog_id":"NEA_38","catalog_name":"GEM_NE_Asia","name":"Har-Us-Nuur Fault","slip_type":"Dextral","reference":"DEM; Gregory et al., 2014","epistemic_quality":"1","accuracy":"60000","activity_confidence":"1","strike_slip_rate":"(2.4,2.0,2.8)","exposure_quality":"1","notes":"Slip rate from Gregory"},{"average_dip":"(90,,)","average_rake":"(135,90,112.5)","catalog_id":"NEA_39","catalog_name":"GEM_NE_Asia","name":"Har-Us-Nuur Fault","slip_type":"Dextral-Reverse","reference":"DEM; Nissen et al. 2009","epistemic_quality":"1","accuracy":"60000","activity_confidence":"1","strike_slip_rate":"(2.4,2.0,2.8)","exposure_quality":"1","notes":"Slip rate from Gregory"},{"average_dip":"(60,50,60)","average_rake":"(90,,)","catalog_id":"NEA_40","catalog_name":"GEM_NE_Asia","dip_dir":"W","name":"Zereg Fault","net_slip_rate":"(0.4,0.23,0.88)","slip_type":"Reverse","reference":"Nissen et al. 2009","epistemic_quality":"1","accuracy":"45000","activity_confidence":"1","downthrown_side_dir":"E","exposure_quality":"1"},{"average_dip":"(30,15,45)","average_rake":"(90,,)","catalog_id":"NEA_41","catalog_name":"GEM_NE_Asia","dip_dir":"E","name":"Altun Huhey Uul Fault","slip_type":"Reverse","reference":"DEM; Frankel et al. 2010","epistemic_quality":"1","accuracy":"40000","activity_confidence":"1","downthrown_side_dir":"W","exposure_quality":"1"},{"average_dip":"(30,20,60)","average_rake":"(90,,)","catalog_id":"NEA_42","catalog_name":"GEM_NE_Asia","dip_dir":"E","slip_type":"Reverse","reference":"DEM; Frankel et al. 2010","epistemic_quality":"1","accuracy":"50000","activity_confidence":"1","downthrown_side_dir":"W","exposure_quality":"1"},{"average_dip":"(90,70,90)","average_rake":"(180,157.5,180)","catalog_id":"NEA_43","catalog_name":"GEM_NE_Asia","dip_dir":"E","name":"Hoh Serh Fault","net_slip_rate":"(0.8,0.7,1.0)","slip_type":"Dextral","reference":"DEM; Frankel et al. 2010","epistemic_quality":"1","accuracy":"60000","activity_confidence":"1","exposure_quality":"1","notes":"Some geomorphic and field evidence for a reverse slip component"},{"average_dip":"(90,,)","catalog_id":"NEA_44","catalog_name":"GEM_NE_Asia","name":"West Sayan Fault","slip_type":"Sinistral","reference":"DEM","epistemic_quality":"2","accuracy":"150000","activity_confidence":"1","exposure_quality":"2"},{"average_dip":"(90,,)","catalog_id":"NEA_45","catalog_name":"GEM_NE_Asia","name":"West Sayan Fault","slip_type":"Sinistral","reference":"DEM","epistemic_quality":"2","accuracy":"180000","activity_confidence":"2","exposure_quality":"2","notes":"very rough interpreted segment in between more evident segments."},{"average_dip":"(90,,)","catalog_id":"NEA_46","catalog_name":"GEM_NE_Asia","slip_type":"Sinistral","reference":"DEM, Google Earth","epistemic_quality":"1","accuracy":"70000","activity_confidence":"1","exposure_quality":"2","notes":"Some OK quaternary scarps in landsat/google earth"},{"average_dip":"(90,,)","catalog_id":"NEA_47","catalog_name":"GEM_NE_Asia","slip_type":"Sinistral","reference":"DEM; Google Earth","epistemic_quality":"1","accuracy":"70000","activity_confidence":"1","exposure_quality":"1"},{"average_dip":"(55,45,70)","catalog_id":"NEA_48","catalog_name":"GEM_NE_Asia","dip_dir":"E","slip_type":"Normal","reference":"DEM","epistemic_quality":"1","accuracy":"90000","activity_confidence":"1","downthrown_side_dir":"E","exposure_quality":"1"},{"average_dip":"(60,45,75)","catalog_id":"NEA_49","catalog_name":"GEM_NE_Asia","dip_dir":"E","slip_type":"Normal","reference":"DEM; Google Earth","epistemic_quality":"2","accuracy":"90000","activity_confidence":"1","downthrown_side_dir":"E","exposure_quality":"1","notes":"Strange but well-defined scarp w/ some imagery evidence for quaternary offsets. May have a significant component of strike-slip, kinematics currently unknown."},{"average_dip":"(50,45,65)","catalog_id":"NEA_50","catalog_name":"GEM_NE_Asia","dip_dir":"W","slip_type":"Normal","reference":"DEM, seismicity","epistemic_quality":"1","accuracy":"90000","activity_confidence":"1","downthrown_side_dir":"W","exposure_quality":"2"},{"average_dip":"(55,45,65)","catalog_id":"NEA_51","catalog_name":"GEM_NE_Asia","dip_dir":"W","slip_type":"Normal","reference":"DEM, Seismicity","epistemic_quality":"1","accuracy":"90000","activity_confidence":"1","downthrown_side_dir":"W","exposure_quality":"2"},{"average_dip":"(55,45,70)","catalog_id":"NEA_52","catalog_name":"GEM_NE_Asia","dip_dir":"E","slip_type":"Normal","reference":"DEM","epistemic_quality":"2","accuracy":"100000","activity_confidence":"2","downthrown_side_dir":"E","exposure_quality":"2"},{"average_dip":"(15,10,40)","catalog_id":"NEA_54","catalog_name":"GEM_NE_Asia","dip_dir":"N","name":"Fuyun Fault, southern endcap","slip_type":"Reverse","reference":"Klinger et al., 2011","epistemic_quality":"1","accuracy":"20000","activity_confidence":"1","fs_name":"Fuyun Fault","exposure_quality":"1","notes":"Really strange reverse fault at end of dextral fault"},{"average_dip":"(90,,)","catalog_id":"NEA_55","catalog_name":"GEM_NE_Asia","name":"Fuyun Fault, south central segment","slip_type":"Dextral","reference":"Klinger et al. 2011","epistemic_quality":"1","accuracy":"20000","activity_confidence":"1","fs_name":"Fuyun Fault","last_movement":"1931","exposure_quality":"1","notes":"Beautiful tectonic geomorphology"},{"average_dip":"(90,,)","catalog_id":"NEA_56","catalog_name":"GEM_NE_Asia","name":"Fuyun Fault Splay","slip_type":"Dextral","reference":"Klinger et al., 2011","epistemic_quality":"1","accuracy":"20000","activity_confidence":"1","fs_name":"Fuyun Fault","last_movement":"1931","exposure_quality":"1","notes":"Splay from 1931 rupture"},{"average_dip":"(90,,)","catalog_id":"NEA_57","catalog_name":"GEM_NE_Asia","name":"Fuyun Fault, Central Segment","slip_type":"Dextral","reference":"Klinger et al. 2011","epistemic_quality":"1","accuracy":"20000","activity_confidence":"1","fs_name":"Fuyun Fault","last_movement":"1931","exposure_quality":"1","notes":"1931 rupture. ~6 , displacement per event over past  5 events."},{"average_dip":"(75,60,90)","catalog_id":"NEA_58","catalog_name":"GEM_NE_Asia","dip_dir":"E","name":"Fuyun Fault, north segment","slip_type":"Dextral-Normal","reference":"Klinger et al. 2011","epistemic_quality":"1","accuracy":"50000","activity_confidence":"1","fs_name":"Fuyun Fault","last_movement":"1931","downthrown_side_dir":"E","exposure_quality":"1"},{"average_dip":"(75,65,90)","catalog_id":"NEA_59","catalog_name":"GEM_NE_Asia","dip_dir":"E","name":"Fuyun Fault, north central segment","slip_type":"Dextral-Normal","reference":"Klinger et al., 2011","epistemic_quality":"1","accuracy":"50000","activity_confidence":"1","fs_name":"Fuyun Fault","last_movement":"1931","downthrown_side_dir":"E","exposure_quality":"1"},{"average_dip":"(70,60,90)","catalog_id":"NEA_60","catalog_name":"GEM_NE_Asia","dip_dir":"E","name":"Khoton Nuur Fault","slip_type":"Dextral-Normal","reference":"Gregory 2012 Explorers Club report","epistemic_quality":"2","accuracy":"100000","activity_confidence":"1","fs_name":"Khoton Nuur Fault","downthrown_side_dir":"E","exposure_quality":"2","notes":"Only mapped in a small figure in a grant proposal report; nothing peer-reviewed yet. Laura Gregory mapped there and did a slip rate study, though. Hard to see the fault in the imagery, but the fault zone is obvious and there is a focal mechanism."},{"average_dip":"(80,70,90)","catalog_id":"NEA_70","catalog_name":"GEM_NE_Asia","dip_dir":"E","name":"Khoton Nuur Fault (south segments)","slip_type":"Dextral-Normal","reference":"Gregory 2012 Explorers Club report","accuracy":"150000","activity_confidence":"1","fs_name":"Khoton Nuur Fault","downthrown_side_dir":"E","notes":"Only mapped in a small figure in a grant proposal report; nothing peer-reviewed yet. Laura Gregory mapped there and did a slip rate study, though. Hard to see the fault in the imagery, but the fault zone is obvious and there is a focal mechanism."},{"average_dip":"(30,15,50)","catalog_id":"NEA_71","catalog_name":"GEM_NE_Asia","dip_dir":"E","name":"Tolbo Nuur Fault","slip_type":"Reverse","reference":"Gregory et al., 2014","epistemic_quality":"1","accuracy":"100000","activity_confidence":"1","fs_name":"Tolbo Nuur Fault","downthrown_side_dir":"W","exposure_quality":"1","notes":"Merges into the strike-slip fault segment to the east."},{"average_dip":"(90,,)","catalog_id":"NEA_72","catalog_name":"GEM_NE_Asia","name":"Tolbo Nuur Fault (strike-slip segment)","slip_type":"Dextral","reference":"Gregory et al., 2014","epistemic_quality":"1","accuracy":"50000","activity_confidence":"1","strike_slip_rate":"(0.9, 0.8, 1.1)","exposure_quality":"1","notes":"Slip rate from cosmogenics. In agreement with Frankel et al. 2011 site 100 km farther south."},{"average_dip":"(30,15,50)","catalog_id":"NEA_73","catalog_name":"GEM_NE_Asia","dip_dir":"N","slip_type":"Reverse","reference":"DEM","epistemic_quality":"1","accuracy":"70000","activity_confidence":"2","downthrown_side_dir":"S","exposure_quality":"1","notes":"Looks like a reverse-bound basin in the DEM. Also mapped by Gregory in a figure but who knows if anyone went there.  Possible fault scarp in Google Earth."},{"average_dip":"(35,20,55)","catalog_id":"NEA_74","catalog_name":"GEM_NE_Asia","dip_dir":"E","slip_type":"Reverse","reference":"DEM","epistemic_quality":"2","accuracy":"80000","activity_confidence":"1","downthrown_side_dir":"W","exposure_quality":"1","notes":"May be northern, contractional continuation of Olgiy Fault. There is a small thrust focal mechanism at the southeast end and the basin looks actively subsiding.  May have a dextral component."},{"average_dip":"(90,,)","catalog_id":"NEA_75","catalog_name":"GEM_NE_Asia","name":"Sagsay Fault","slip_type":"Dextral","reference":"DEM; Gregory et al. 2014","epistemic_quality":"1","accuracy":"80000","activity_confidence":"1","fs_name":"Sagsay Fault","exposure_quality":"1","notes":"Gregory shows it to continue to north and south for ~100 km but I can't find it clearly"},{"average_dip":"(45,20,60)","catalog_id":"NEA_76","catalog_name":"GEM_NE_Asia","dip_dir":"W","name":"Tsetseg Fault","slip_type":"Reverse-Dextral","reference":"DEM; Cunningham et al., 1996","epistemic_quality":"1","accuracy":"80000","activity_confidence":"1","downthrown_side_dir":"E","exposure_quality":"1","notes":"Nice basin in DEM. Peculiar that fault daylights so high up the bajada but that seems to be how the ALtai work."},{"average_dip":"(90,,)","catalog_id":"NEA_77","catalog_name":"GEM_NE_Asia","name":"Sagsay Fault (north segment)","slip_type":"Dextral","reference":"Google Earth; DEM; Gregory 2010","epistemic_quality":"1","accuracy":"80000","activity_confidence":"1","exposure_quality":"1","notes":"Earthquke rupture very clear in Google Earth."},{"average_dip":"(70,40,90)","catalog_id":"NEA_78","catalog_name":"GEM_NE_Asia","dip_dir":"E","name":"Turgin Gol Fault","slip_type":"Dextral-Reverse","reference":"DEM; Cunningham et al. 1996","epistemic_quality":"1","accuracy":"60000","activity_confidence":"1","downthrown_side_dir":"W","exposure_quality":"1","notes":"Dip and rake covary with strike. N-segments are probably vertical/dextral, and NW-striking segmentts dip towards high topography and have a reverse component."},{"average_dip":"(90,,)","catalog_id":"NEA_83","catalog_name":"GEM_NE_Asia","name":"Bulgan Gol Fault (eastern segment)","slip_type":"Sinistral","reference":"Baljinnyam et al., 1993; DEM; Google Earth","epistemic_quality":"1","accuracy":"50000","activity_confidence":"1","exposure_quality":"1","notes":"Well defined fault between other sinistral-ish fault segments. Not a lot of sign of Quaternary activity on it, but the trace is clear and it is surrounded by similar active faults. Imagery is a little bad."},{"average_dip":"(90,,)","catalog_id":"NEA_79","catalog_name":"GEM_NE_Asia","slip_type":"Sinistral","reference":"Google Earth","epistemic_quality":"1","accuracy":"30000","activity_confidence":"1","exposure_quality":"1","notes":"Found on Google EArth. Good stepover geomorphology."},{"average_dip":"(90,,)","catalog_id":"NEA_80","catalog_name":"GEM_NE_Asia","name":"Baruum-Hurray Fault (western segment)","slip_type":"Sinistral","reference":"Baljinnyam et al., 1993; Google Earth","epistemic_quality":"1","accuracy":"30000","activity_confidence":"1","exposure_quality":"1","notes":"Long rupture observed (and inferred in places) in Google Earth.  Taylor 2010 puts a fault through here too, probably based on SRTM 90."},{"average_dip":"(90,,)","catalog_id":"NEA_81","catalog_name":"GEM_NE_Asia","name":"Baruum-Huuray Fault (eastern segment)","slip_type":"Sinistral","reference":"Baljinnyam et al., 1993; Google Earth","epistemic_quality":"1","accuracy":"50000","activity_confidence":"2","exposure_quality":"1","notes":"Mapped in Google Earth. It is the eastern half of a long fault that is clearly active in the west, but more ambiguous here. The imagery is worse. Merges with other faults in the high southern Altai."},{"average_dip":"(90,,)","catalog_id":"NEA_82","catalog_name":"GEM_NE_Asia","name":"Bulgan Gol fault (western segment)","slip_type":"Sinistral","reference":"Google Earth","epistemic_quality":"1","accuracy":"30000","activity_confidence":"1","exposure_quality":"1","notes":"Rupture mapped in Google Earth. Continues eastward but quaternary activity east of this structure is unclear."},{"average_dip":"(80,60,90)","catalog_id":"NEA_85","catalog_name":"GEM_NE_Asia","dip_dir":"W","name":"Tonhil Fault (north segment)","slip_type":"Dextral","reference":"Baljinnyam et al., 1993; DEM","epistemic_quality":"1","accuracy":"30000","activity_confidence":"1","downthrown_side_dir":"E","exposure_quality":"1","notes":"this segment has a  nice visible rupture in google earth"},{"average_dip":"(90,,)","catalog_id":"NEA_86","catalog_name":"GEM_NE_Asia","name":"Tonhil Fault, south section","slip_type":"Dextral","reference":"Baljinnyam et al., 1993; Google Earth; DEM","epistemic_quality":"1","accuracy":"50000","activity_confidence":"1","exposure_quality":"1","notes":"Good visible rupture (or at least fault trace) over much of the fault"},{"average_dip":"(30,20,50)","catalog_id":"NEA_87","catalog_name":"GEM_NE_Asia","dip_dir":"E","slip_type":"Reverse","reference":"DEM","epistemic_quality":"1","accuracy":"50000","activity_confidence":"1","downthrown_side_dir":"W","exposure_quality":"1"},{"average_dip":"(40,20,70)","catalog_id":"NEA_88","catalog_name":"GEM_NE_Asia","dip_dir":"NE","slip_type":"Reverse-Dextral","reference":"DEM; Cunningham faults","epistemic_quality":"1","accuracy":"50000","activity_confidence":"1","downthrown_side_dir":"SW","exposure_quality":"1","notes":"Well expressed in DEM, but poor imagery and no clear signes of Quartnary rupture. Activity may be shifted to younger-looking faults to the SE."},{"average_dip":"(45,30,60)","catalog_id":"NEA_61","catalog_name":"GEM_NE_Asia","dip_dir":"E","slip_type":"Reverse-Dextral","reference":"DEM; Google Earth","epistemic_quality":"2","accuracy":"50000","activity_confidence":"2","downthrown_side_dir":"W","exposure_quality":"1","notes":"Possibly active, possibly no longer active. Imagery is poor but clear in the topography."},{"average_dip":"(45,20,60)","catalog_id":"NEA_62","catalog_name":"GEM_NE_Asia","dip_dir":"E","slip_type":"Dextral-Reverse","reference":"DEM; Cunningham faults","epistemic_quality":"2","accuracy":"100000","activity_confidence":"2","downthrown_side_dir":"W","exposure_quality":"2","notes":"Ambiguous in terms of Quaternary activity, but clearly an old transpressional fault"},{"average_dip":"(90,,)","catalog_id":"NEA_63","catalog_name":"GEM_NE_Asia","slip_type":"Dextral","reference":"DEM; Cunningham faults","epistemic_quality":"1","accuracy":"50000","activity_confidence":"1","exposure_quality":"1","notes":"Strange structure. Looks like the eastern margin of a transpressional pop-up, but at the soutehrn end there is a clear grabe where there is transtension at a stepover; strcuture is probably not vertical (looks west-dipping) but hard to say with that graben."},{"average_dip":"(60,40,90)","catalog_id":"NEA_64","catalog_name":"GEM_NE_Asia","dip_dir":"W","slip_type":"Dextral-Oblique","reference":"DEM; Cunningham faults","epistemic_quality":"1","accuracy":"50000","activity_confidence":"1","downthrown_side_dir":"E","exposure_quality":"1"},{"average_dip":"(60,40,90)","catalog_id":"NEA_65","catalog_name":"GEM_NE_Asia","dip_dir":"E","slip_type":"Dextral-Reverse","reference":"DEM","epistemic_quality":"1","accuracy":"60000","activity_confidence":"1","downthrown_side_dir":"W","exposure_quality":"1"},{"average_dip":"(60,40,90)","catalog_id":"NEA_66","catalog_name":"GEM_NE_Asia","dip_dir":"E","slip_type":"Dextral-Reverse","reference":"DEM","epistemic_quality":"1","accuracy":"60000","activity_confidence":"1","downthrown_side_dir":"W","exposure_quality":"1"},{"average_dip":"(30,20,50)","catalog_id":"NEA_67","catalog_name":"GEM_NE_Asia","dip_dir":"NE","slip_type":"Reverse","reference":"DEM","epistemic_quality":"1","accuracy":"50000","activity_confidence":"1","downthrown_side_dir":"SW","exposure_quality":"1","notes":"Beautiful on DEM. Almost certainly merges with main thrust to NE."},{"average_dip":"(30,20,60)","catalog_id":"NEA_68","catalog_name":"GEM_NE_Asia","dip_dir":"W","slip_type":"Reverse","reference":"DEM; Google Earth","epistemic_quality":"1","accuracy":"60000","activity_confidence":"1","downthrown_side_dir":"E","exposure_quality":"1","notes":"Very strange, probably misoriented but very clear reverse(?) fault. Uplift of the east at least is clear."},{"average_dip":"(60,40,75)","catalog_id":"NEA_69","catalog_name":"GEM_NE_Asia","dip_dir":"E","slip_type":"Dextral-Reverse","reference":"DEM","epistemic_quality":"2","accuracy":"100000","activity_confidence":"2","downthrown_side_dir":"W","exposure_quality":"1","notes":"This, or a similar nearby structure, clearly bounds a huge transpressional popup (2.5 km relief) and transfers dextral slip along N-S faults ot the north to the east-striking faults to the east. But it's not clear exactly where the surface expression of it is, or how active. I am picking this arrangement but I am a bit uncertain."},{"average_dip":"(90,,)","catalog_id":"NEA_89","catalog_name":"GEM_NE_Asia","slip_type":"Dextral","reference":"DEM","epistemic_quality":"2","accuracy":"70000","activity_confidence":"2","exposure_quality":"1","notes":"Good tectonic geomorphology indicating a dextral fault, but may be old."},{"average_dip":"(40,20,60)","catalog_id":"NEA_90","catalog_name":"GEM_NE_Asia","dip_dir":"NE","slip_type":"Reverse","reference":"DEM","epistemic_quality":"1","accuracy":"60000","activity_confidence":"1","downthrown_side_dir":"SW","exposure_quality":"1"},{"average_dip":"(40,20,60)","catalog_id":"NEA_91","catalog_name":"GEM_NE_Asia","dip_dir":"NE","slip_type":"Reverse","reference":"DEM","epistemic_quality":"1","accuracy":"50000","activity_confidence":"1","downthrown_side_dir":"SW","exposure_quality":"1"},{"average_dip":"(90,,)","catalog_id":"NEA_92","catalog_name":"GEM_NE_Asia","slip_type":"Sinistral","reference":"DEM; Google Earth","epistemic_quality":"1","accuracy":"20000","activity_confidence":"1","exposure_quality":"1","notes":"Clear rupture in Google Earth"},{"average_dip":"(90,,)","catalog_id":"NEA_93","catalog_name":"GEM_NE_Asia","name":"Tahiynshar Fault","slip_type":"Sinistral","reference":"Googe Earth; Khil'ko 1985","epistemic_quality":"1","accuracy":"20000","activity_confidence":"1","last_movement":"1974","exposure_quality":"1","notes":"Rupture in google earth probably is that mapped by Khil'ko (1985) of teh 1974 Tahiynshar M~7 easrthquake."},{"average_dip":"(60,20,70)","catalog_id":"NEA_94","catalog_name":"GEM_NE_Asia","dip_dir":"N","slip_type":"Sinistral-Reverse","reference":"DEM; Cunningham Faults","epistemic_quality":"1","accuracy":"20000","activity_confidence":"1","downthrown_side_dir":"S","exposure_quality":"1","notes":"Good rupture visible especially in strike-slip segments"},{"average_dip":"(70,40,90)","catalog_id":"NEA_95","catalog_name":"GEM_NE_Asia","dip_dir":"NE","name":"Sutay Uul Fault","slip_type":"Dextral-Reverse","reference":"DEM; Cunningham Faults","epistemic_quality":"1","accuracy":"50000","activity_confidence":"2","downthrown_side_dir":"SW","exposure_quality":"1"},{"average_dip":"(70,30,90)","catalog_id":"NEA_102","catalog_name":"GEM_NE_Asia","dip_dir":"N","slip_type":"Sinistral-Reverse","reference":"DEM; Cunningham Faults","epistemic_quality":"1","accuracy":"100000","activity_confidence":"1","exposure_quality":"1","notes":"Connects more visible ruptures"},{"average_dip":"(70,40,80)","catalog_id":"NEA_103","catalog_name":"GEM_NE_Asia","dip_dir":"NE","name":"Ich Obo Fault","slip_type":"Dextral-Reverse","reference":"Cunningham Faults; DEM","epistemic_quality":"1","accuracy":"65000","activity_confidence":"1","downthrown_side_dir":"SW","exposure_quality":"1","notes":"sure puts up some big mountains"},{"average_dip":"(90,,)","catalog_id":"NEA_96","catalog_name":"GEM_NE_Asia","slip_type":"Sinistral","reference":"DEM; Cunningham Faults","epistemic_quality":"1","accuracy":"50000","activity_confidence":"1","exposure_quality":"1","notes":"pretty curved for a strike-slip fault."},{"average_dip":"(30,20,50)","catalog_id":"NEA_97","catalog_name":"GEM_NE_Asia","dip_dir":"SW","name":"North Shargyn Thrust","slip_type":"Reverse","reference":"DEM; Cunningham Faults","epistemic_quality":"1","accuracy":"30000","activity_confidence":"1","downthrown_side_dir":"NE","exposure_quality":"1","notes":"May have another name and some description in the literature, but I can't qui"},{"average_dip":"(90,,)","catalog_id":"NEA_98","catalog_name":"GEM_NE_Asia","name":"Shargyn Fault","slip_type":"Sinistral","reference":"Baljinnyam et al., 1993; Cunningham Faults","epistemic_quality":"1","accuracy":"30000","activity_confidence":"1","exposure_quality":"1"},{"average_dip":"(20,15,40)","catalog_id":"NEA_99","catalog_name":"GEM_NE_Asia","dip_dir":"N","name":"Buuralyn Nuruu Thrust North","slip_type":"Reverse","reference":"Baljinnyam et al., 1993; Cunningham Faults","epistemic_quality":"1","accuracy":"30000","activity_confidence":"1","downthrown_side_dir":"S","exposure_quality":"1"},{"average_dip":"(20,15,40)","catalog_id":"NEA_100","catalog_name":"GEM_NE_Asia","dip_dir":"E","name":"Buuralyn Nuruu Thrust East","slip_type":"Reverse","reference":"Baljinnyam et al., 1993; Cunningham Faults","epistemic_quality":"1","accuracy":"30000","activity_confidence":"1","downthrown_side_dir":"W","exposure_quality":"1"},{"average_dip":"(20,15,40)","catalog_id":"NEA_101","catalog_name":"GEM_NE_Asia","dip_dir":"E","name":"Buuralyn Nuruu Thrust SE","slip_type":"Reverse","reference":"DEM; Cunningham Faults","epistemic_quality":"1","accuracy":"50000","activity_confidence":"1","downthrown_side_dir":"W","exposure_quality":"1"},{"average_dip":"(70,40,80)","catalog_id":"NEA_30","catalog_name":"GEM_NE_Asia","dip_dir":"N","slip_type":"Sinistral-Reverse","reference":"DEM","epistemic_quality":"1","accuracy":"30000","activity_confidence":"1","downthrown_side_dir":"S","exposure_quality":"1","notes":"Some rupture visible in Google Earth"},{"average_dip":"(70,40,80)","catalog_id":"NEA_104","catalog_name":"GEM_NE_Asia","dip_dir":"N","slip_type":"Sinistral-Reverse","reference":"DEM","epistemic_quality":"1","accuracy":"35000","activity_confidence":"1","downthrown_side_dir":"S","exposure_quality":"1"},{"average_dip":"(90,,)","catalog_id":"NEA_105","catalog_name":"GEM_NE_Asia","slip_type":"Sinistral","reference":"DEM; Cunningham Faults","epistemic_quality":"1","accuracy":"50000","activity_confidence":"1","exposure_quality":"1"},{"average_dip":"(90,,)","catalog_id":"NEA_106","catalog_name":"GEM_NE_Asia","slip_type":"Sinistral","reference":"DEM","epistemic_quality":"1","accuracy":"40000","activity_confidence":"2","exposure_quality":"1"},{"average_dip":"(50,20,70)","catalog_id":"NEA_107","catalog_name":"GEM_NE_Asia","dip_dir":"NE","slip_type":"Reverse","reference":"DEM; Cunningham Faults","epistemic_quality":"1","accuracy":"40000","activity_confidence":"1","downthrown_side_dir":"SW","exposure_quality":"1","notes":"Some offset of Quaternary seds visible, and it looks like only reverse offset. However it's quite long and straight so it looks like it might be a reactivated strike-slip or oblique-slip fault, not a primary low-angle thrust."},{"average_dip":"(90,,)","catalog_id":"NEA_108","catalog_name":"GEM_NE_Asia","name":"Bugat Fault","slip_type":"Sinistral","reference":"DEM","epistemic_quality":"1","accuracy":"60000","activity_confidence":"1","exposure_quality":"1"},{"average_dip":"(20,15,40)","catalog_id":"NEA_109","catalog_name":"GEM_NE_Asia","dip_dir":"S","name":"Togrog Gol Thrust","slip_type":"Reverse","reference":"Baljinnyam et al., 1993; Cunningham Faults","epistemic_quality":"1","accuracy":"50000","activity_confidence":"1","downthrown_side_dir":"N","exposure_quality":"1"},{"average_dip":"(45,20,60)","catalog_id":"NEA_110","catalog_name":"GEM_NE_Asia","dip_dir":"S","slip_type":"Reverse","reference":"DEM; Cunningham Faults","epistemic_quality":"1","accuracy":"40000","activity_confidence":"2","downthrown_side_dir":"N","exposure_quality":"1","notes":"Looks increasingly less active towards the east and at the rangefront"},{"average_dip":"(40,30,70)","catalog_id":"NEA_111","catalog_name":"GEM_NE_Asia","dip_dir":"S","slip_type":"Reverse","reference":"DEM; Cunningham Faults","epistemic_quality":"1","accuracy":"60000","activity_confidence":"1","downthrown_side_dir":"N","exposure_quality":"1","notes":"Looks steeper and less active to the E"},{"average_dip":"(30,15,50)","catalog_id":"NEA_112","catalog_name":"GEM_NE_Asia","dip_dir":"N","slip_type":"Reverse","reference":"DEM; Cunningham Faults","epistemic_quality":"1","accuracy":"40000","activity_confidence":"1","downthrown_side_dir":"S","exposure_quality":"1"},{"average_dip":"(90,,)","catalog_id":"NEA_113","catalog_name":"GEM_NE_Asia","slip_type":"Sinistral","reference":"DEM; Cunningham Faults","epistemic_quality":"1","accuracy":"40000","activity_confidence":"1","exposure_quality":"1"},{"average_dip":"(90,,)","catalog_id":"NEA_114","catalog_name":"GEM_NE_Asia","slip_type":"Sinistral","reference":"DEM; Cunningham Faults","epistemic_quality":"1","accuracy":"30000","activity_confidence":"1","exposure_quality":"1","notes":"Baljinnyam et al. find ~1 m scarp in field survey and moderate dips."},{"average_dip":"(50,40,60)","catalog_id":"NEA_115","catalog_name":"GEM_NE_Asia","dip_dir":"N","name":"Hasagt Haryan FAult","slip_type":"Reverse-Sinistral","reference":"Baljinnyam et al., 1993; Cunningham Faults","epistemic_quality":"1","accuracy":"30000","activity_confidence":"1","downthrown_side_dir":"S","exposure_quality":"1"},{"average_dip":"(30,15,50)","catalog_id":"NEA_116","catalog_name":"GEM_NE_Asia","dip_dir":"S","slip_type":"Reverse","reference":"Cunningham Faults","epistemic_quality":"1","accuracy":"60000","activity_confidence":"1","downthrown_side_dir":"N","exposure_quality":"1"},{"average_dip":"(30,20,50)","catalog_id":"NEA_117","catalog_name":"GEM_NE_Asia","dip_dir":"S","slip_type":"Reverse","reference":"DEM; Cunningham Faults","epistemic_quality":"1","accuracy":"80000","activity_confidence":"1","downthrown_side_dir":"N","exposure_quality":"1"},{"average_dip":"(90,,)","catalog_id":"NEA_118","catalog_name":"GEM_NE_Asia","name":"Chandman Fault","slip_type":"Sinistral","reference":"Baljinnyam et al., 1993","epistemic_quality":"1","accuracy":"30000","activity_confidence":"1","exposure_quality":"1","notes":"~1 m characteristic offsets from field recon"},{"average_dip":"(90,,)","average_rake":"","catalog_id":"NEA_119","catalog_name":"GEM_NE_Asia","name":"Myangayn Fault","slip_type":"Reverse","reference":"Baljinnyam et al., 1993","epistemic_quality":"1","accuracy":"30000","activity_confidence":"1","exposure_quality":"1"},{"average_dip":"(90,70,90)","catalog_id":"NEA_120","catalog_name":"GEM_NE_Asia","dip_dir":"S","slip_type":"Sinistral","reference":"DEM; Cunningham Faults","epistemic_quality":"1","accuracy":"70000","activity_confidence":"1","downthrown_side_dir":"N","exposure_quality":"1","notes":"may have some reverse component, throwing south side up"},{"average_dip":"(90,,)","catalog_id":"NEA_121","catalog_name":"GEM_NE_Asia","slip_type":"Sinistral","reference":"DEM","epistemic_quality":"1","accuracy":"70000","activity_confidence":"1","exposure_quality":"1"},{"average_dip":"(50,40,90)","catalog_id":"NEA_122","catalog_name":"GEM_NE_Asia","dip_dir":"S","slip_type":"Sinistral-Reverse","reference":"DEM","epistemic_quality":"1","accuracy":"30000","activity_confidence":"1","downthrown_side_dir":"N","exposure_quality":"1","notes":"Reverse fault probably reactivated to sinistral. Dipping fault visible in Google Earth."},{"average_dip":"(90,,)","catalog_id":"NEA_123","catalog_name":"GEM_NE_Asia","slip_type":"Sinistral","reference":"DEM; Cunningham Faults","epistemic_quality":"1","accuracy":"30000","activity_confidence":"1","exposure_quality":"1"},{"average_dip":"(60,40,90)","catalog_id":"NEA_124","catalog_name":"GEM_NE_Asia","dip_dir":"S","slip_type":"Sinistral","reference":"DEM; Cunningham Faults","epistemic_quality":"1","accuracy":"30000","activity_confidence":"1","downthrown_side_dir":"N","exposure_quality":"1","notes":"S dip based on geomorphology and imagery, but slip is probably nearly pure sinistral with revers partitioned to the north"},{"average_dip":"(90,70,90)","catalog_id":"NEA_125","catalog_name":"GEM_NE_Asia","dip_dir":"S","name":"Bogd Fault (west segment)","slip_type":"Sinistral","reference":"Baljinnyam et al., 1993; Choi et al., 2012; Ritz et al., 1995","epistemic_quality":"1","accuracy":"30000","activity_confidence":"1","last_movement":"1957","downthrown_side_dir":"N","strike_slip_rate":"(1.2,,)","exposure_quality":"1","notes":"Western segment of 1957 Gobi-Altai Rupture"},{"average_dip":"(25,15,50)","catalog_id":"NEA_126","catalog_name":"GEM_NE_Asia","dip_dir":"S","name":"North Il Bogd Thrust","slip_type":"Sinistral-Reverse","reference":"Baljinnyam et al., 1993; Choi et al., 2012; Ritz et al., 1995","epistemic_quality":"1","accuracy":"30000","activity_confidence":"1","last_movement":"1957","downthrown_side_dir":"N","strike_slip_rate":"(1.2,,)","exposure_quality":"1","notes":"Part of 1957 rupture. I put the main sinistral slip rate from Ritz 1995 on this fault although it's likely that most of the sinistral slip is at the rangefront and this is essentially a pure thrust fault with a much slower rate."},{"average_dip":"(90,70,90)","catalog_id":"NEA_127","catalog_name":"GEM_NE_Asia","dip_dir":"S","name":"Bogd Fault (central segment)","slip_type":"Sinistral","reference":"Baljinnyam et al., 1993; Choi et al., 2012; Ritz et al., 1995","epistemic_quality":"1","accuracy":"30000","activity_confidence":"1","last_movement":"1957","downthrown_side_dir":"N","strike_slip_rate":"(1.2,,)","exposure_quality":"1","notes":"Central segment of 1957 rupture."},{"average_dip":"(70,50,90)","catalog_id":"NEA_129","catalog_name":"GEM_NE_Asia","dip_dir":"S","name":"Bogd Fault (eastern segment)","slip_type":"Sinistral-Reverse","reference":"Baljinnyam et al., 1993; Choi et al., 2012; Ritz et al., 1995","epistemic_quality":"1","accuracy":"30000","activity_confidence":"1","last_movement":"1957","downthrown_side_dir":"N","strike_slip_rate":"(1.2,,)","exposure_quality":"1","notes":"Eastern segment of 1957 rupture"},{"average_dip":"(25,15,40)","catalog_id":"NEA_130","catalog_name":"GEM_NE_Asia","dip_dir":"N","name":"Gurvan Bulag Thrust","slip_type":"Reverse","reference":"ritz et al., 2003; Bayarsayhan et al., 1996; Prentice et al., 2002","epistemic_quality":"1","accuracy":"30000","activity_confidence":"1","last_movement":"1957","downthrown_side_dir":"S","vert_sep_rate":"(0.44, 0.11, 1.3)","exposure_quality":"1","notes":"Visible rupture from 1957 earthquake in google earth"},{"average_dip":"(90,,)","catalog_id":"NEA_131","catalog_name":"GEM_NE_Asia","slip_type":"Sinistral","epistemic_quality":"1","accuracy":"50000","activity_confidence":"1","exposure_quality":"1","notes":"650 km long strike-slip fault, continuous in Google Earth. Poorly studied and kind of terrifying."},{"average_dip":"(50,40,70)","catalog_id":"NEA_128","catalog_name":"GEM_NE_Asia","dip_dir":"N","name":"Egiin Davaa","net_slip_rate":"(1.,0.04,1.)","slip_type":"Normal","reference":"Walker et al., 2017","epistemic_quality":"1","accuracy":"50000","activity_confidence":"1","downthrown_side_dir":"N","exposure_quality":"1","notes":"Walker found evidence for 1-2 earthquakes over the last 16 ka, with 8 m of vertical displacement, yielding ~1 mm/yr dip slip. However, there is only 225 m of total offset on a 6 Ma basalt, yielding a late Neogene rate of 0.04 mm/yr. The faster rate is preferred as it more accurately describes the current slip regime."},{"average_dip":"(50,45,70)","catalog_id":"NEA_132","catalog_name":"GEM_NE_Asia","dip_dir":"NW","name":"Egiin Davaa East","slip_type":"Normal","reference":"DEM","epistemic_quality":"1","accuracy":"70000","activity_confidence":"2","downthrown_side_dir":"NW","exposure_quality":"1","notes":""},{"average_dip":"(50,40,70)","catalog_id":"NEA_133","catalog_name":"GEM_NE_Asia","dip_dir":"SE","name":"Mandal Fault","slip_type":"Normal","reference":"SW shown in Walker et al, 2017; NE mapped in DEM","epistemic_quality":"1","accuracy":"50000","activity_confidence":"1","downthrown_side_dir":"SE","exposure_quality":"1"},{"average_dip":"(70,40,80)","catalog_id":"NEA_134","catalog_name":"GEM_NE_Asia","dip_dir":"E","name":"Otgon Fault","slip_type":"Normal-Dextral","reference":"DEM; Cunningham Faults","epistemic_quality":"1","accuracy":"50000","activity_confidence":"1","downthrown_side_dir":"E","exposure_quality":"1","notes":"It looks too steep just to be a normal fault, and there is a little jog in the fault just south of where I stopped mapping that switches dip direction but is consistent with dextral slip."},{"average_dip":"(90,,)","catalog_id":"NEA_135","catalog_name":"GEM_NE_Asia","slip_type":"Sinistral","reference":"DEM; Cunningham Faults","epistemic_quality":"1","accuracy":"50000","activity_confidence":"1","exposure_quality":"1","notes":"super clear ruptures in google earth"},{"average_dip":"(35,20,50)","catalog_id":"NEA_136","catalog_name":"GEM_NE_Asia","dip_dir":"W","name":"Bayan Hongor Fault","slip_type":"Reverse","reference":"Walker et al., 2007","epistemic_quality":"1","accuracy":"60000","activity_confidence":"1","downthrown_side_dir":"E","exposure_quality":"1","notes":"Claimed to be a reverse fault by Walker, though Cunningham (early on) claimed it as normal. Reverse makes more sense but it kind of looks normal. Probably steep and reactivated in any case, not a nice low-angle detachment thrust."},{"average_dip":"(90,,)","catalog_id":"NEA_137","catalog_name":"GEM_NE_Asia","name":"Bayan Bulag Fault","slip_type":"Sinistral","reference":"DEM; Cunningham Faults; Walker et al., 2007","epistemic_quality":"1","accuracy":"30000","activity_confidence":"1","exposure_quality":"1","notes":"Has transpressional sections, but shown as purely sinistral by Walker in center."},{"average_dip":"(90,,)","catalog_id":"NEA_138","catalog_name":"GEM_NE_Asia","name":"Khujirt Fault","slip_type":"Dextral","reference":"DEM","epistemic_quality":"1","accuracy":"60000","activity_confidence":"1","exposure_quality":"1","notes":"Part of a longer dextral (?) system; occasionally well experssed, sometimes less so."},{"average_dip":"(90,,)","catalog_id":"NEA_139","catalog_name":"GEM_NE_Asia","name":"Ulziit Fault","slip_type":"Dextral","reference":"DEM; Cunningham Faults","epistemic_quality":"1","accuracy":"50000","activity_confidence":"1","exposure_quality":"1","notes":"Looks like dextral based on extensional stepover geometry."},{"average_dip":"(90,,)","catalog_id":"NEA_140","catalog_name":"GEM_NE_Asia","slip_type":"Dextral","reference":"DEM; Cunningham Faults","epistemic_quality":"1","accuracy":"50000","activity_confidence":"1","exposure_quality":"1"},{"average_dip":"(90,,)","catalog_id":"NEA_141","catalog_name":"GEM_NE_Asia","name":"Tavanbulag Fault","slip_type":"Dextral","reference":"DEM; Google Earth","epistemic_quality":"1","accuracy":"50000","activity_confidence":"2","exposure_quality":"1","notes":"Mapped based on imagery; not seen in literature. Parth of long dextral ? system from Tsetserleg to Gobi."},{"average_dip":"(90,,)","catalog_id":"NEA_142","catalog_name":"GEM_NE_Asia","slip_type":"Dextral","reference":"DEM; Google Earth","epistemic_quality":"1","accuracy":"50000","activity_confidence":"2","exposure_quality":"1"},{"average_dip":"(90,,)","catalog_id":"NEA_143","catalog_name":"GEM_NE_Asia","name":"West Khujirt Fault","slip_type":"Dextral","reference":"DEM; Google Earth","epistemic_quality":"1","accuracy":"50000","activity_confidence":"2","exposure_quality":"1"},{"average_dip":"(50,40,65)","catalog_id":"NEA_144","catalog_name":"GEM_NE_Asia","dip_dir":"NW","name":"Bat Ultzii Fault","slip_type":"Normal","reference":"DEM; Google Earth","epistemic_quality":"1","accuracy":"50000","activity_confidence":"1","downthrown_side_dir":"NW","exposure_quality":"1","notes":"Surely written about in a paper somewhere, but it's obvious enough in the imagery"},{"average_dip":"(90,,)","catalog_id":"NEA_145","catalog_name":"GEM_NE_Asia","name":"Teregtiin Fault","slip_type":"Dextral","reference":"Schlupp and Cisternas, 2007","epistemic_quality":"1","accuracy":"40000","activity_confidence":"1","last_movement":"1905","exposure_quality":"1","notes":"Conjugate rupture to Bolnay 1905"},{"average_dip":"(90,60,90)","catalog_id":"NEA_146","catalog_name":"GEM_NE_Asia","dip_dir":"NW","name":"Tsetserleg Fault","slip_type":"Sinistral-Reverse","reference":"Schlupp and Cisternas, 2007","epistemic_quality":"1","accuracy":"50000","activity_confidence":"1","downthrown_side_dir":"SE","exposure_quality":"1","notes":"1905 Tsetserleg rupture. Schlupp and Cisternas indicate S-directed overthrusting on part of it, but this is not super clear in Google EArth or the large-scale topography."},{"average_dip":"(65,40,90)","catalog_id":"NEA_147","catalog_name":"GEM_NE_Asia","dip_dir":"W","slip_type":"Dextral-Reverse","reference":"DEM","epistemic_quality":"1","accuracy":"60000","activity_confidence":"1","fs_name":"Uzhep Fault System","downthrown_side_dir":"E","exposure_quality":"2","notes":"This is the northern part of a long (~100 km) N-S fault ; a few moderate earthquakes (6.7, 6.6) in 2011-2012 probably reactivated the northern end and are dextral and reverse-dextral.  Additional information is unknown but I haven't searched in depth. "},{"average_dip":"(65,40,90)","catalog_id":"NEA_148","catalog_name":"GEM_NE_Asia","dip_dir":"E","slip_type":"Dextral-Normal","reference":"DEM","epistemic_quality":"2","accuracy":"60000","activity_confidence":"2","fs_name":"Uzhep Fault System","downthrown_side_dir":"E","exposure_quality":"2","notes":"Southern part of a ~100 km long N-S fault. Focal mechs and to some degree fault geomorphology suggest toe north is dextral-reverse, but this segemnt  looks dextral-normal (triangular facets  etc."},{"average_dip":"(20,15,35)","catalog_id":"NEA_149","catalog_name":"GEM_NE_Asia","dip_dir":"N","slip_type":"Reverse","reference":"DEM","epistemic_quality":"1","accuracy":"80000","activity_confidence":"1","downthrown_side_dir":"S","exposure_quality":"1"},{"average_dip":"(20,15,35)","catalog_id":"NEA_150","catalog_name":"GEM_NE_Asia","dip_dir":"N","slip_type":"Reverse","reference":"DEM","epistemic_quality":"1","accuracy":"90000","activity_confidence":"1","downthrown_side_dir":"S","exposure_quality":"1"},{"average_dip":"(90,,)","catalog_id":"NEA_151","catalog_name":"GEM_NE_Asia","slip_type":"Sinistral","reference":"DEM","epistemic_quality":"1","accuracy":"40000","activity_confidence":"1","exposure_quality":"2","notes":"Amazing sinistral bedrock offsets"},{"average_dip":"(50,45,60)","catalog_id":"NEA_152","catalog_name":"GEM_NE_Asia","dip_dir":"W","slip_type":"Normal","reference":"DEM","epistemic_quality":"1","accuracy":"80000","activity_confidence":"1","downthrown_side_dir":"W","exposure_quality":"2","notes":"Possible dextral offsets as well, particularly between large terminal moraine on south end and rangefront."},{"average_dip":"(50,45,60)","catalog_id":"NEA_153","catalog_name":"GEM_NE_Asia","dip_dir":"W","slip_type":"Normal","reference":"DEM","epistemic_quality":"1","accuracy":"50000","activity_confidence":"1","downthrown_side_dir":"W","exposure_quality":"2","notes":"Incredibly beautiful area; I want to goooooooo"},{"average_dip":"(50,45,60)","catalog_id":"NEA_154","catalog_name":"GEM_NE_Asia","dip_dir":"E","name":"Khovsgol Fault","slip_type":"Normal","reference":"DEM","epistemic_quality":"1","accuracy":"80000","activity_confidence":"1","downthrown_side_dir":"E","exposure_quality":"2"},{"average_dip":"(90,,)","catalog_id":"NEA_155","catalog_name":"GEM_NE_Asia","name":"Azas-Sentsa Fault","slip_type":"Sinistral","reference":"Arzhannikova et al., 2011; DEM","epistemic_quality":"1","accuracy":"60000","activity_confidence":"1","exposure_quality":"2","notes":"Western half has excellent rupture visible in SRTM, for km after km. When the fault gets into the mountains and is in a long glacial valley, this fades but the linearity of the valley makes it obvious where the fault is."},{"average_dip":"(90,,)","catalog_id":"NEA_156","catalog_name":"GEM_NE_Asia","name":"Central Sayan Fault","slip_type":"Sinistral","reference":"DEM","epistemic_quality":"1","accuracy":"120000","activity_confidence":"2","exposure_quality":"2","notes":"Clear bedrock fault, but Quaternary activity is uncertain. In many cases it looks like geomorphic features are cut but obvious offsets with consisten kinematics are lacking.  However, imagery is not great, so this relies only on SRTM."},{"average_dip":"(90,,)","catalog_id":"NEA_157","catalog_name":"GEM_NE_Asia","name":"Gunzhin Fault","reference":"Imaev et al., 2012; Demberel et al., 2014","epistemic_quality":"2","accuracy":"70000","activity_confidence":"1","exposure_quality":"2","notes":"General location and kinematics from Imaev and Demberel. Hard to accurately map on the ground, and kinematics are unclear. Nonetheless, they document deformation (folding and fissuring, no clear faulting) in a trench with 1-2 Holocene paleoearthquakes.  They consider the fault to be Dextral but that isn't very clear from the topography or the regional tectonics."},{"average_dip":"(30,20,50)","catalog_id":"NEA_158","catalog_name":"GEM_NE_Asia","dip_dir":"E","name":"Emeelt Fault","slip_type":"Reverse-Dextral","reference":"Dujardin et al., 2014; Seminsky et al., 2017","epistemic_quality":"1","accuracy":"30000","activity_confidence":"1","downthrown_side_dir":"W","exposure_quality":"1","notes":"Visible scarp in Google Earth for center of fault, where it was trnched by Dujardin and colleagues. The trace is extended to the north and south based on seismicity.  Dextral offset is inferred based on GPR surveys, and reverse component based on estimated dip and striek w/r/t regional strain field."},{"average_dip":"(60,40,70)","catalog_id":"NEA_159","catalog_name":"GEM_NE_Asia","dip_dir":"S","slip_type":"Normal","reference":"DEM","epistemic_quality":"1","accuracy":"150000","activity_confidence":"1","downthrown_side_dir":"S","exposure_quality":"1","notes":"Could have a sinistral component"},{"average_dip":"(70,40,80)","catalog_id":"NEA_160","catalog_name":"GEM_NE_Asia","dip_dir":"N","name":"Mondy Fault","slip_type":"Sinistral-Normal","reference":"DEM; Lunina Faults","epistemic_quality":"1","accuracy":"35000","activity_confidence":"1","downthrown_side_dir":"N","exposure_quality":"1"},{"average_dip":"(50,45,60)","catalog_id":"NEA_161","catalog_name":"GEM_NE_Asia","dip_dir":"S","name":"Tunka Fault","slip_type":"Normal","reference":"DEM; Lunina Faults","epistemic_quality":"1","accuracy":"35000","activity_confidence":"1","downthrown_side_dir":"S","exposure_quality":"1","notes":"gorgeous"},{"average_dip":"(90,,)","catalog_id":"NEA_162","catalog_name":"GEM_NE_Asia","name":"South Main Sayan Fault","slip_type":"Sinistral","reference":"DEM","epistemic_quality":"1","accuracy":"100000","activity_confidence":"1","exposure_quality":"2","notes":"Looks more active to SE"},{"average_dip":"(90,,)","catalog_id":"NEA_163","catalog_name":"GEM_NE_Asia","name":"Oka-Jombolok Fault","slip_type":"Sinistral","reference":"DEM","epistemic_quality":"1","accuracy":"60000","activity_confidence":"1","exposure_quality":"2","notes":"Western half has excellent rupture visible in SRTM, for km after km. When the fault gets into the mountains and is in a long glacial valley, this fades but the linearity of the valley makes it obvious where the fault is."},{"average_dip":"(90,,)","catalog_id":"NEA_164","catalog_name":"GEM_NE_Asia","name":"Yamaatinskiy Fault","slip_type":"Sinistral","reference":"Arzhannikova et al., 2011; DEM","epistemic_quality":"1","accuracy":"150000","activity_confidence":"2","exposure_quality":"2"},{"average_dip":"(90,,)","catalog_id":"NEA_165","catalog_name":"GEM_NE_Asia","name":"NE Erzin-Agar-Dag Fault","slip_type":"Sinistral","reference":"DEM","epistemic_quality":"1","accuracy":"60000","activity_confidence":"1","exposure_quality":"2"},{"average_dip":"(25,15,45)","catalog_id":"NEA_166","catalog_name":"GEM_NE_Asia","dip_dir":"NW","name":"Hustai Fault","slip_type":"Reverse","reference":"Ferry et al., 2010; Demberel et al., 2014","epistemic_quality":"1","accuracy":"60000","activity_confidence":"1","downthrown_side_dir":"SE","exposure_quality":"1","notes":"Ferry states this is the central segment of a much longer fault. Very clear ruptures in the imagery here."},{"average_dip":"(90,,)","catalog_id":"NEA_167","catalog_name":"GEM_NE_Asia","slip_type":"Sinistral","reference":"DEM; Google Earth","epistemic_quality":"1","accuracy":"60000","activity_confidence":"2","exposure_quality":"1","notes":"Good but discontinuous ruptures visible in GE. Looks to be sinistrael."},{"average_dip":"(90,,)","catalog_id":"NEA_168","catalog_name":"GEM_NE_Asia","slip_type":"Sinistral","reference":"DEM; Google Earth","epistemic_quality":"1","accuracy":"60000","activity_confidence":"2","exposure_quality":"1","notes":"Good rupture visibility in GE."},{"average_dip":"(90,,)","catalog_id":"NEA_169","catalog_name":"GEM_NE_Asia","slip_type":"Sinistral","reference":"Google Earth; DEM","epistemic_quality":"1","accuracy":"60000","activity_confidence":"2","exposure_quality":"1","notes":"Good rupture visibility in GE."},{"average_dip":"(50,40,65)","catalog_id":"NEA_170","catalog_name":"GEM_NE_Asia","dip_dir":"N","name":"South Baikal Fault","slip_type":"Normal","reference":"DEM; Lunina Faults","epistemic_quality":"1","accuracy":"40000","activity_confidence":"1","downthrown_side_dir":"N","exposure_quality":"2","notes":"Fault in main Baikal rift hanging wall"},{"average_dip":"(50,40,65)","catalog_id":"NEA_171","catalog_name":"GEM_NE_Asia","dip_dir":"NW","name":"Chersky Fault","slip_type":"Normal","reference":"DEM; Lunina Faults","epistemic_quality":"1","accuracy":"70000","activity_confidence":"1","downthrown_side_dir":"NW","exposure_quality":"2"},{"average_dip":"(50,40,60)","catalog_id":"NEA_172","catalog_name":"GEM_NE_Asia","dip_dir":"S","name":"Obruchev Fault","slip_type":"Normal","reference":"Lunina Faults; Google Earth bathymetry","epistemic_quality":"1","accuracy":"100000","activity_confidence":"1","downthrown_side_dir":"S","exposure_quality":"3","notes":"Trace mapped underwater in coarse bathymetry."},{"average_dip":"(50,40,60)","catalog_id":"NEA_173","catalog_name":"GEM_NE_Asia","dip_dir":"E","name":"Primorsky Fault","slip_type":"Normal","reference":"Google Earth; Lunina Faults","epistemic_quality":"1","accuracy":"100000","activity_confidence":"1","downthrown_side_dir":"E","exposure_quality":"3","notes":"Major Baikal structure"},{"average_dip":"(50,40,60)","catalog_id":"NEA_174","catalog_name":"GEM_NE_Asia","dip_dir":"E","name":"Morsky Faults","slip_type":"Normal","reference":"Lunina Faults; DEM","epistemic_quality":"1","accuracy":"100000","activity_confidence":"1","downthrown_side_dir":"E","exposure_quality":"3"},{"average_dip":"(50,40,60)","catalog_id":"NEA_175","catalog_name":"GEM_NE_Asia","dip_dir":"E","name":"Kocherikovsky Fault","slip_type":"Normal","reference":"Lunina Faults; Google Earth Bathymetry","epistemic_quality":"1","accuracy":"100000","activity_confidence":"1","downthrown_side_dir":"E","exposure_quality":"3"},{"average_dip":"(50,40,60)","catalog_id":"NEA_176","catalog_name":"GEM_NE_Asia","dip_dir":"E","slip_type":"Normal","reference":"Lunina Faults; Google Earth Bathymetry","epistemic_quality":"1","accuracy":"100000","activity_confidence":"1","downthrown_side_dir":"E","exposure_quality":"3"},{"average_dip":"(50,40,60)","catalog_id":"NEA_177","catalog_name":"GEM_NE_Asia","dip_dir":"SE","slip_type":"Normal","reference":"Lunina Faults; DEM","epistemic_quality":"1","accuracy":"90000","activity_confidence":"1","downthrown_side_dir":"SE","exposure_quality":"1"},{"average_dip":"(50,40,60)","catalog_id":"NEA_178","catalog_name":"GEM_NE_Asia","dip_dir":"NW","slip_type":"Normal","reference":"Lunina Faults; DEM","epistemic_quality":"1","accuracy":"50000","activity_confidence":"1","downthrown_side_dir":"NW","exposure_quality":"1","notes":"Bangin' facets"},{"average_dip":"(50,40,60)","catalog_id":"NEA_179","catalog_name":"GEM_NE_Asia","dip_dir":"NW","slip_type":"Normal","reference":"Lunina Faults; DEM","epistemic_quality":"1","accuracy":"50000","activity_confidence":"1","downthrown_side_dir":"NW","exposure_quality":"1"},{"average_dip":"(50,40,60)","catalog_id":"NEA_180","catalog_name":"GEM_NE_Asia","dip_dir":"SE","slip_type":"Normal","reference":"Lunina Faults; DEM","epistemic_quality":"1","accuracy":"60000","activity_confidence":"1","downthrown_side_dir":"SE","exposure_quality":"1"},{"average_dip":"(50,40,60)","catalog_id":"NEA_182","catalog_name":"GEM_NE_Asia","dip_dir":"E","slip_type":"Normal","reference":"Lunina Faults; DEM","epistemic_quality":"1","accuracy":"90000","activity_confidence":"1","downthrown_side_dir":"E","exposure_quality":"1"},{"average_dip":"(50,40,60)","catalog_id":"NEA_181","catalog_name":"GEM_NE_Asia","dip_dir":"E","slip_type":"Normal","reference":"Lunina Faults; DEM","epistemic_quality":"1","accuracy":"80000","activity_confidence":"1","downthrown_side_dir":"E","exposure_quality":"1"},{"average_dip":"(50,40,60)","catalog_id":"NEA_183","catalog_name":"GEM_NE_Asia","dip_dir":"W","slip_type":"Normal","reference":"Lunina Faults; DEM","epistemic_quality":"1","accuracy":"60000","activity_confidence":"1","downthrown_side_dir":"W","exposure_quality":"1"},{"average_dip":"(50,40,60)","catalog_id":"NEA_184","catalog_name":"GEM_NE_Asia","dip_dir":"S","slip_type":"Normal","reference":"Lunina Faults; DEM","epistemic_quality":"1","accuracy":"150000","activity_confidence":"1","downthrown_side_dir":"S","exposure_quality":"1"},{"average_dip":"(50,40,60)","catalog_id":"NEA_185","catalog_name":"GEM_NE_Asia","dip_dir":"S","slip_type":"Normal","reference":"Lunina Faults; DEM","epistemic_quality":"1","accuracy":"50000","activity_confidence":"1","downthrown_side_dir":"S","exposure_quality":"1","notes":"Great scarp"},{"average_dip":"(50,40,60)","catalog_id":"NEA_186","catalog_name":"GEM_NE_Asia","dip_dir":"NW","slip_type":"Normal","reference":"DEM","epistemic_quality":"1","accuracy":"60000","activity_confidence":"1","downthrown_side_dir":"NW","exposure_quality":"1"},{"average_dip":"(50,40,60)","catalog_id":"NEA_187","catalog_name":"GEM_NE_Asia","dip_dir":"S","slip_type":"Normal","reference":"DEM","epistemic_quality":"1","accuracy":"50000","activity_confidence":"1","downthrown_side_dir":"S","exposure_quality":"1","notes":"Good scarp in Google Earth"},{"average_dip":"(50,40,60)","catalog_id":"NEA_188","catalog_name":"GEM_NE_Asia","dip_dir":"S","slip_type":"Normal","reference":"DEM","epistemic_quality":"1","accuracy":"50000","activity_confidence":"1","downthrown_side_dir":"S","exposure_quality":"1","notes":"Pretty amazing ponding of rivers at the rangefront"},{"average_dip":"(50,40,60)","catalog_id":"NEA_189","catalog_name":"GEM_NE_Asia","dip_dir":"NW","slip_type":"Normal","reference":"Lunina Faults; DEM","epistemic_quality":"1","accuracy":"60000","activity_confidence":"1","downthrown_side_dir":"NW","exposure_quality":"1"},{"average_dip":"(50,40,60)","catalog_id":"NEA_190","catalog_name":"GEM_NE_Asia","dip_dir":"NW","slip_type":"Normal","reference":"DEM","epistemic_quality":"1","accuracy":"50000","activity_confidence":"1","downthrown_side_dir":"NW","exposure_quality":"1"},{"average_dip":"(50,40,60)","catalog_id":"NEA_191","catalog_name":"GEM_NE_Asia","dip_dir":"N","slip_type":"Normal","reference":"DEM","epistemic_quality":"1","accuracy":"60000","activity_confidence":"1","downthrown_side_dir":"N","exposure_quality":"1"},{"average_dip":"(50,40,60)","catalog_id":"NEA_192","catalog_name":"GEM_NE_Asia","dip_dir":"SE","slip_type":"Normal","reference":"DEM","epistemic_quality":"1","accuracy":"50000","activity_confidence":"1","downthrown_side_dir":"SE","exposure_quality":"1"},{"average_dip":"(50,40,60)","catalog_id":"NEA_193","catalog_name":"GEM_NE_Asia","dip_dir":"NW","slip_type":"Normal","reference":"DEM","epistemic_quality":"1","accuracy":"45000","activity_confidence":"1","downthrown_side_dir":"NW","exposure_quality":"1"},{"average_dip":"(60,50,70)","catalog_id":"NEA_194","catalog_name":"GEM_NE_Asia","dip_dir":"SE","slip_type":"Normal-Sinistral","reference":"DEM","epistemic_quality":"1","accuracy":"50000","activity_confidence":"1","downthrown_side_dir":"SE","exposure_quality":"1"},{"average_dip":"(60,50,70)","catalog_id":"NEA_195","catalog_name":"GEM_NE_Asia","dip_dir":"NW","slip_type":"Normal-Sinistral","reference":"DEM","epistemic_quality":"1","accuracy":"50000","activity_confidence":"1","downthrown_side_dir":"NW","exposure_quality":"1"},{"average_dip":"(60,40,70)","catalog_id":"NEA_196","catalog_name":"GEM_NE_Asia","dip_dir":"E","slip_type":"Normal","reference":"DEM","epistemic_quality":"2","accuracy":"100000","activity_confidence":"2","downthrown_side_dir":"E","exposure_quality":"2","notes":"Could be normal-oblique.  Hard to make out kinematics here."},{"average_dip":"(60,40,70)","catalog_id":"NEA_197","catalog_name":"GEM_NE_Asia","dip_dir":"SE","slip_type":"Normal-Sinistral","reference":"DEM","epistemic_quality":"1","accuracy":"100000","activity_confidence":"2","downthrown_side_dir":"SE","exposure_quality":"1","notes":"Kinematics are a guess, but fault is clear in landscape"},{"average_dip":"(50,40,60)","catalog_id":"NEA_198","catalog_name":"GEM_NE_Asia","dip_dir":"S","slip_type":"Normal","reference":"DEM","epistemic_quality":"1","accuracy":"150000","activity_confidence":"2","downthrown_side_dir":"S","exposure_quality":"2","notes":"Possible fault hosting a cluster of similarly-oriented normal faulting earthquakes in late 2011"},{"average_dip":"(60,40,70)","catalog_id":"NEA_199","catalog_name":"GEM_NE_Asia","dip_dir":"E","slip_type":"Dextral-Normal","reference":"DEM","epistemic_quality":"1","accuracy":"150000","activity_confidence":"2","downthrown_side_dir":"E","exposure_quality":"1","notes":"Nice exposure in the DEM; activity (and to a lesser degree, kinematics) uncertain."},{"average_dip":"(65,50,75)","catalog_id":"NEA_200","catalog_name":"GEM_NE_Asia","dip_dir":"W","slip_type":"Dextral-Normal","reference":"DEM","epistemic_quality":"2","accuracy":"100000","activity_confidence":"2","downthrown_side_dir":"W","exposure_quality":"2","notes":"Lots of uplift, possible ruptures in landsat."},{"average_dip":"(50,40,60)","catalog_id":"NEA_201","catalog_name":"GEM_NE_Asia","dip_dir":"S","slip_type":"Normal","reference":"DEM","epistemic_quality":"1","accuracy":"200000","activity_confidence":"2","downthrown_side_dir":"S","exposure_quality":"2","notes":"Uplift along this fault, but when?"},{"average_dip":"(90,60,90)","catalog_id":"NEA_202","catalog_name":"GEM_NE_Asia","dip_dir":"S","slip_type":"Sinistral","reference":"DEM","epistemic_quality":"2","accuracy":"250000","activity_confidence":"2","downthrown_side_dir":"S","exposure_quality":"2","notes":"Somewhere within a few hundred km, there is ~1mm/yr of sinistral slip. This looks like the most likely location."},{"average_dip":"(90,,)","catalog_id":"NEA_203","catalog_name":"GEM_NE_Asia","slip_type":"Sinistral","reference":"DEM","epistemic_quality":"1","accuracy":"150000","activity_confidence":"1","exposure_quality":"1","notes":"Slightly better sign of activity and trace than adjacent segment to NW, but still poor."},{"average_dip":"(90,,)","catalog_id":"NEA_204","catalog_name":"GEM_NE_Asia","slip_type":"Sinistral","reference":"DEM","epistemic_quality":"2","accuracy":"100000","activity_confidence":"2","exposure_quality":"2"},{"average_dip":"(90,,)","catalog_id":"NEA_205","catalog_name":"GEM_NE_Asia","slip_type":"Sinistral","reference":"DEM","epistemic_quality":"1","accuracy":"100000","activity_confidence":"1","exposure_quality":"2","notes":"Looks a bit more active than neighbors to W. But where does it go to the E?"},{"average_dip":"(90,,)","catalog_id":"NEA_206","catalog_name":"GEM_NE_Asia","slip_type":"Sinistral","reference":"DEM","epistemic_quality":"1","accuracy":"100000","activity_confidence":"1","exposure_quality":"1","notes":"Most convincing tectonic geomorphology east of Baikal"},{"average_dip":"(50,40,70)","catalog_id":"NEA_207","catalog_name":"GEM_NE_Asia","dip_dir":"N","slip_type":"Normal-Sinistral","reference":"DEM","epistemic_quality":"1","accuracy":"60000","activity_confidence":"1","downthrown_side_dir":"N","exposure_quality":"1","notes":"Nice basalts in hanging wall.  Maybe not sinistral(?)  Normal faulting is based on what look like very nice triangular facets."},{"average_dip":"(90,,)","catalog_id":"NEA_208","catalog_name":"GEM_NE_Asia","slip_type":"Sinistral","reference":"DEM","epistemic_quality":"1","accuracy":"100000","activity_confidence":"1","exposure_quality":"1","notes":"Cool little connector fault"},{"average_dip":"(90,,)","catalog_id":"NEA_209","catalog_name":"GEM_NE_Asia","slip_type":"Sinistral","reference":"DEM","epistemic_quality":"2","accuracy":"200000","activity_confidence":"2","exposure_quality":"2","notes":"Firm maybe"},{"average_dip":"(90,60,90)","catalog_id":"NEA_210","catalog_name":"GEM_NE_Asia","dip_dir":"S","slip_type":"Sinistral-Normal","reference":"DEM","epistemic_quality":"2","accuracy":"150000","activity_confidence":"2","downthrown_side_dir":"S","exposure_quality":"1","notes":"Some sort of scarp in the landscape, but it might be bedding. Nonetheless there is abundant seismicity and there must be a fault around here somewhere."},{"average_dip":"(90,,)","catalog_id":"NEA_211","catalog_name":"GEM_NE_Asia","slip_type":"Sinistral","reference":"DEM","epistemic_quality":"2","accuracy":"200000","activity_confidence":"2","exposure_quality":"2","notes":"Very scant evidence for faulting here, but seismicity in the region does exist, and this is as likely a candidate fault as any."},{"average_dip":"(90,,)","catalog_id":"NEA_212","catalog_name":"GEM_NE_Asia","slip_type":"Sinistral","reference":"DEM","epistemic_quality":"2","accuracy":"100000","activity_confidence":"2","exposure_quality":"2","notes":"Good exposure in west, then gets less clear, but a lineament is obvious."},{"average_dip":"(90,,)","catalog_id":"NEA_213","catalog_name":"GEM_NE_Asia","slip_type":"Sinistral","reference":"DEM","epistemic_quality":"2","accuracy":"150000","activity_confidence":"2","exposure_quality":"2","notes":"Looks possible"},{"average_dip":"(90,,)","catalog_id":"NEA_214","catalog_name":"GEM_NE_Asia","slip_type":"Sinistral","reference":"DEM","epistemic_quality":"1","accuracy":"100000","activity_confidence":"1","exposure_quality":"1","notes":"Especially convincing (for this region) sinistral offsets at western end"},{"average_dip":"(90,,)","catalog_id":"NEA_215","catalog_name":"GEM_NE_Asia","slip_type":"Sinistral","reference":"DEM","epistemic_quality":"2","accuracy":"200000","activity_confidence":"2","exposure_quality":"2","notes":"Some OK evidence for deformation. Also the bumps in the topography kind of look like a volcanic field."},{"average_dip":"(90,,)","catalog_id":"NEA_216","catalog_name":"GEM_NE_Asia","slip_type":"Sinistral","epistemic_quality":"2","accuracy":"900000","activity_confidence":"2","exposure_quality":"2","notes":"This is the most likely place for a fault connecting the easetern and western segments of the Amuria-Eurasia plate boundary, but little evidence exists for a fault right here other than this wide valley in between two probable faults."},{"average_dip":"(90,,)","catalog_id":"NEA_217","catalog_name":"GEM_NE_Asia","slip_type":"Sinistral","reference":"DEM","epistemic_quality":"1","accuracy":"60000","activity_confidence":"1","exposure_quality":"1"},{"average_dip":"(90,,)","catalog_id":"NEA_218","catalog_name":"GEM_NE_Asia","slip_type":"Sinistral","reference":"DEM","epistemic_quality":"1","accuracy":"100000","activity_confidence":"2","exposure_quality":"2","notes":"Good looking fault, may not be active"},{"average_dip":"(20,15,30)","catalog_id":"NEA_219","catalog_name":"GEM_NE_Asia","dip_dir":"W","slip_type":"Reverse","reference":"DEM","epistemic_quality":"2","accuracy":"150000","activity_confidence":"2","downthrown_side_dir":"E","exposure_quality":"2"},{"average_dip":"(90,,)","catalog_id":"NEA_220","catalog_name":"GEM_NE_Asia","slip_type":"Sinistral","reference":"DEM","epistemic_quality":"2","accuracy":"150000","activity_confidence":"2","exposure_quality":"2"},{"average_dip":"(20,15,30)","catalog_id":"NEA_221","catalog_name":"GEM_NE_Asia","dip_dir":"W","slip_type":"Reverse","reference":"DEM","epistemic_quality":"2","accuracy":"150000","activity_confidence":"2","downthrown_side_dir":"E","exposure_quality":"2"},{"average_dip":"(20,15,30)","catalog_id":"NEA_222","catalog_name":"GEM_NE_Asia","dip_dir":"W","slip_type":"Reverse","reference":"DEM","epistemic_quality":"2","accuracy":"200000","activity_confidence":"2","downthrown_side_dir":"E","exposure_quality":"2"},{"average_dip":"(20,15,30)","catalog_id":"NEA_223","catalog_name":"GEM_NE_Asia","dip_dir":"W","slip_type":"Reverse","reference":"DEM","epistemic_quality":"2","accuracy":"200000","activity_confidence":"2","downthrown_side_dir":"E","exposure_quality":"2"},{"average_dip":"(20,150,30)","catalog_id":"NEA_224","catalog_name":"GEM_NE_Asia","dip_dir":"W","slip_type":"Reverse","reference":"DEM","epistemic_quality":"2","accuracy":"300000","activity_confidence":"2","downthrown_side_dir":"E","exposure_quality":"2"},{"average_dip":"(20,15,30)","catalog_id":"NEA_225","catalog_name":"GEM_NE_Asia","dip_dir":"W","slip_type":"Reverse","reference":"DEM","epistemic_quality":"2","accuracy":"250000","activity_confidence":"2","downthrown_side_dir":"E","exposure_quality":"2"},{"average_dip":"(20,15,30)","catalog_id":"NEA_226","catalog_name":"GEM_NE_Asia","dip_dir":"W","slip_type":"Reverse","reference":"DEM","epistemic_quality":"2","accuracy":"250000","activity_confidence":"2","downthrown_side_dir":"E","exposure_quality":"2"},{"average_dip":"(25,20,40)","catalog_id":"NEA_227","catalog_name":"GEM_NE_Asia","dip_dir":"W","name":"Pobeda Thrust","slip_type":"Reverse","reference":"DEM","epistemic_quality":"1","accuracy":"150000","activity_confidence":"1","downthrown_side_dir":"E","exposure_quality":"2"},{"average_dip":"(20,15,30)","catalog_id":"NEA_228","catalog_name":"GEM_NE_Asia","dip_dir":"W","name":"North Pobeda Thrust","slip_type":"Reverse","reference":"DEM","epistemic_quality":"1","accuracy":"150000","activity_confidence":"1","downthrown_side_dir":"E","exposure_quality":"1"},{"average_dip":"(90,,)","catalog_id":"NEA_229","catalog_name":"GEM_NE_Asia","name":"SE Ulakhan Fault","slip_type":"Sinistral","reference":"Khozurin, 2004","epistemic_quality":"1","accuracy":"30000","activity_confidence":"1","exposure_quality":"1","notes":"Good sign of rupture through entire trace"},{"average_dip":"(20,15,40)","catalog_id":"NEA_230","catalog_name":"GEM_NE_Asia","dip_dir":"SW","name":"NW Momsky Thrust","slip_type":"Reverse","reference":"DEM","epistemic_quality":"1","accuracy":"50000","activity_confidence":"1","downthrown_side_dir":"NE","exposure_quality":"1"},{"average_dip":"(20,15,40)","catalog_id":"NEA_231","catalog_name":"GEM_NE_Asia","dip_dir":"SW","name":"SE Pobeda Thrust","slip_type":"Reverse","reference":"DEM","epistemic_quality":"1","accuracy":"50000","activity_confidence":"1","downthrown_side_dir":"NE","exposure_quality":"1"},{"average_dip":"(90,,)","catalog_id":"NEA_232","catalog_name":"GEM_NE_Asia","name":"North Central Ulakhan Fault","slip_type":"Sinistral","reference":"DEM; Khozurin, 2004","epistemic_quality":"1","accuracy":"50000","activity_confidence":"1","exposure_quality":"1","notes":"Less obvious activity than SE segment"},{"average_dip":"(90,,)","catalog_id":"NEA_233","catalog_name":"GEM_NE_Asia","slip_type":"Sinistral","reference":"DEM; Khozurin, 2004","epistemic_quality":"1","accuracy":"60000","activity_confidence":"2","exposure_quality":"2","notes":"Might be active; evidence ambiguous in imagery."},{"average_dip":"(90,,)","catalog_id":"NEA_289","catalog_name":"GEM_NE_Asia","name":"Lankovaya_1","slip_type":"Dextral","reference":"DEM; Khozurin, 2004","epistemic_quality":"1","accuracy":"50000","activity_confidence":"1","exposure_quality":"1","notes":"good traces in GE and ArcticDEM"},{"average_dip":"(90,,)","catalog_id":"NEA_291","catalog_name":"GEM_NE_Asia","name":"Lankovaya_2","slip_type":"Dextral","reference":"DEM; Khozurin, 2004","epistemic_quality":"1","accuracy":"50000","activity_confidence":"1","exposure_quality":"1"},{"average_dip":"(50,35,65)","catalog_id":"NEA_290","catalog_name":"GEM_NE_Asia","dip_dir":"S","slip_type":"Normal","reference":"DEM","epistemic_quality":"1","accuracy":"45000","activity_confidence":"1","downthrown_side_dir":"S","exposure_quality":"1"},{"average_dip":"(50,35,65)","catalog_id":"NEA_286","catalog_name":"GEM_NE_Asia","dip_dir":"S","slip_type":"Normal","reference":"DEM","epistemic_quality":"1","accuracy":"45000","activity_confidence":"1","downthrown_side_dir":"S","exposure_quality":"1"},{"average_dip":"(50,35,65)","catalog_id":"NEA_285","catalog_name":"GEM_NE_Asia","dip_dir":"S","slip_type":"Normal","reference":"DEM","epistemic_quality":"1","accuracy":"45000","activity_confidence":"1","downthrown_side_dir":"S","exposure_quality":"1"},{"average_dip":"(50,35,65)","catalog_id":"NEA_288","catalog_name":"GEM_NE_Asia","dip_dir":"S","slip_type":"Normal","reference":"DEM","epistemic_quality":"1","accuracy":"45000","activity_confidence":"1","downthrown_side_dir":"S","exposure_quality":"1"},{"average_dip":"(50,35,65)","catalog_id":"NEA_287","catalog_name":"GEM_NE_Asia","dip_dir":"S","slip_type":"Normal","reference":"DEM","epistemic_quality":"1","accuracy":"45000","activity_confidence":"1","downthrown_side_dir":"S","exposure_quality":"1"},{"average_dip":"(55,35,65)","catalog_id":"NEA_282","catalog_name":"GEM_NE_Asia","dip_dir":"SE","slip_type":"Normal","reference":"DEM","epistemic_quality":"1","accuracy":"45000","activity_confidence":"1","downthrown_side_dir":"SE","exposure_quality":"2"},{"average_dip":"(50,30,70)","catalog_id":"NEA_281","catalog_name":"GEM_NE_Asia","dip_dir":"W","slip_type":"Normal","reference":"Kozhurin, 2004","epistemic_quality":"1","accuracy":"40000","activity_confidence":"1","fs_name":"East Kamchatka Fault Zone","downthrown_side_dir":"W","exposure_quality":"1"},{"average_dip":"(50,30,70)","catalog_id":"NEA_284","catalog_name":"GEM_NE_Asia","dip_dir":"W","slip_type":"Normal","reference":"Kozhurin, 2004","epistemic_quality":"1","accuracy":"40000","activity_confidence":"1","fs_name":"East Kamchatka Fault Zone","downthrown_side_dir":"W","exposure_quality":"1"},{"average_dip":"(50,30,70)","catalog_id":"NEA_283","catalog_name":"GEM_NE_Asia","dip_dir":"W","slip_type":"Normal","reference":"Google Earth; Khozurin","epistemic_quality":"1","accuracy":"40000","activity_confidence":"1","fs_name":"East Kamchatka Fault Zone","downthrown_side_dir":"W","exposure_quality":"1"},{"average_dip":"(50,30,70)","catalog_id":"NEA_278","catalog_name":"GEM_NE_Asia","dip_dir":"W","slip_type":"Normal","reference":"Google Earth; Khozurin","epistemic_quality":"1","accuracy":"40000","activity_confidence":"1","fs_name":"East Kamchatka Fault Zone","downthrown_side_dir":"W","exposure_quality":"1"},{"average_dip":"(50,30,70)","catalog_id":"NEA_277","catalog_name":"GEM_NE_Asia","dip_dir":"W","slip_type":"Normal","reference":"Google Earth; Khozurin","epistemic_quality":"1","accuracy":"40000","activity_confidence":"1","fs_name":"East Kamchatka Fault Zone","downthrown_side_dir":"W","exposure_quality":"1"},{"average_dip":"(50,30,70)","catalog_id":"NEA_280","catalog_name":"GEM_NE_Asia","dip_dir":"W","slip_type":"Normal","reference":"Google Earth; Khozurin","epistemic_quality":"1","accuracy":"40000","activity_confidence":"1","fs_name":"East Kamchatka Fault Zone","downthrown_side_dir":"W","exposure_quality":"1"},{"average_dip":"(50,30,70)","catalog_id":"NEA_279","catalog_name":"GEM_NE_Asia","dip_dir":"W","slip_type":"Normal","reference":"Kozhurin, 2004","epistemic_quality":"1","accuracy":"40000","activity_confidence":"1","fs_name":"East Kamchatka Fault Zone","downthrown_side_dir":"W","exposure_quality":"1"},{"average_dip":"(50,30,70)","catalog_id":"NEA_274","catalog_name":"GEM_NE_Asia","dip_dir":"W","slip_type":"Normal","reference":"Google Earth; Khozurin","epistemic_quality":"1","accuracy":"40000","activity_confidence":"1","fs_name":"East Kamchatka Fault Zone","downthrown_side_dir":"W","exposure_quality":"1"},{"average_dip":"(50,30,70)","catalog_id":"NEA_273","catalog_name":"GEM_NE_Asia","dip_dir":"W","slip_type":"Normal","reference":"Kozhurin, 2004","epistemic_quality":"1","accuracy":"40000","activity_confidence":"1","fs_name":"East Kamchatka Fault Zone","downthrown_side_dir":"W","exposure_quality":"1"},{"average_dip":"(50,30,70)","catalog_id":"NEA_275","catalog_name":"GEM_NE_Asia","dip_dir":"W","slip_type":"Normal","reference":"Google Earth; Khozurin","epistemic_quality":"1","accuracy":"40000","activity_confidence":"1","fs_name":"East Kamchatka Fault Zone","downthrown_side_dir":"W","exposure_quality":"1"},{"average_dip":"(30,15,40)","catalog_id":"NEA_270","catalog_name":"GEM_NE_Asia","dip_dir":"E","slip_type":"Reverse","reference":"DEM; GCMT","accuracy":"60000","downthrown_side_dir":"W","notes":"Dip based on focal mechanisms"},{"average_dip":"(30,15,40)","catalog_id":"NEA_269","catalog_name":"GEM_NE_Asia","dip_dir":"E","slip_type":"Reverse","reference":"DEM; GCMT","accuracy":"60000","downthrown_side_dir":"W","notes":"Dip based on focal mechanisms"},{"average_dip":"(30,15,40)","catalog_id":"NEA_272","catalog_name":"GEM_NE_Asia","dip_dir":"E","slip_type":"Reverse","reference":"DEM; GCMT","accuracy":"60000","downthrown_side_dir":"W"},{"average_dip":"(85,80,90)","catalog_id":"NEA_271","catalog_name":"GEM_NE_Asia","dip_dir":"NE","name":"Kheyton Fault","slip_type":"Dextral","reference":"Rozhdestvenskiy, 1973","epistemic_quality":"1","accuracy":"50000","activity_confidence":"1","exposure_quality":"1"},{"average_dip":"(85,80,90)","catalog_id":"NEA_266","catalog_name":"GEM_NE_Asia","dip_dir":"NE","name":"Longri Fault","slip_type":"Dextral","reference":"Rozhdestvenskiy, 1973","accuracy":"50000","activity_confidence":"1"},{"average_dip":"(90,,)","catalog_id":"NEA_265","catalog_name":"GEM_NE_Asia","name":"Tuin Fault","slip_type":"Dextral","reference":"Rozhdestvenskiy, 1973","accuracy":"80000","activity_confidence":"1"},{"average_dip":"(90,,)","catalog_id":"NEA_268","catalog_name":"GEM_NE_Asia","name":"Ekhabi-Pil'tun Fault","slip_type":"Dextral","reference":"Tsutsumi et al., 2005; Rogozhin, 1996","epistemic_quality":"1","accuracy":"120000","activity_confidence":"1","last_movement":"<2950 BC","exposure_quality":"2","notes":"May not be located exactly; allow a few km on either side."},{"average_dip":"(35,15,55)","catalog_id":"NEA_267","catalog_name":"GEM_NE_Asia","dip_dir":"W","name":"Tym-Poronaysk Fault","slip_type":"Reverse","reference":"Tsutsumi et al., 2005; Kogan et al., 2003","epistemic_quality":"1","accuracy":"70000","activity_confidence":"1","downthrown_side_dir":"E","exposure_quality":"1","shortening_rate":"(3,,)","notes":"Reverse slip, with some (distributed?) dextral slip in region"},{"average_dip":"(30,15,45)","catalog_id":"NEA_262","catalog_name":"GEM_NE_Asia","dip_dir":"W","name":"South Tym-Poronaysk Fault","slip_type":"Reverse","reference":"Fournier et al., 1994; Tsutsumi et al., 2005","epistemic_quality":"1","accuracy":"80000","activity_confidence":"2","downthrown_side_dir":"E","exposure_quality":"1","shortening_rate":"(1.5, 0, 2)","notes":"May not be active."},{"average_dip":"(15,10,20)","catalog_id":"NEA_261","catalog_name":"GEM_NE_Asia","dip_dir":"SW","slip_type":"Reverse","reference":"Kozhurin, 2004","epistemic_quality":"1","accuracy":"250000","activity_confidence":"1","downthrown_side_dir":"NE","exposure_quality":"2"},{"average_dip":"(90,,)","catalog_id":"NEA_264","catalog_name":"GEM_NE_Asia","slip_type":"Sinistral","reference":"De Grave et al, 2009","epistemic_quality":"2","accuracy":"80000","activity_confidence":"2","fs_name":"West Sayan Fault","exposure_quality":"2","notes":"Looks most convincing in west; may be elsewhere to east"},{"average_dip":"(90,,)","catalog_id":"NEA_263","catalog_name":"GEM_NE_Asia","slip_type":"Sinistral","reference":"Dehandschutter et al, 2002","epistemic_quality":"1","accuracy":"70000","activity_confidence":"2","fs_name":"West Sayan Fault","exposure_quality":"2","notes":"decent expression in DEM"},{"average_dip":"(60,50,70)","catalog_id":"NEA_258","catalog_name":"GEM_NE_Asia","dip_dir":"E","name":"Teletsk Graben","slip_type":"Normal","reference":"Dehandschutter et al, 2002","epistemic_quality":"1","accuracy":"80000","activity_confidence":"1","downthrown_side_dir":"E","exposure_quality":"1"},{"average_dip":"(80,60,90)","catalog_id":"NEA_292","catalog_name":"GEM_NE_Asia","dip_dir":"E","reference":"DEM","epistemic_quality":"1","accuracy":"45000","activity_confidence":"2","downthrown_side_dir":"E","exposure_quality":"1","notes":"Enigmatic but well-expressed structure in topo data."},{"average_dip":"(70,50,80)","catalog_id":"NEA_260","catalog_name":"GEM_NE_Asia","dip_dir":"E","slip_type":"Dextral-Normal","reference":"DEM","epistemic_quality":"1","accuracy":"40000","activity_confidence":"1","downthrown_side_dir":"E","exposure_quality":"1","notes":"Haven't seen in the literature but it's clean as a whistle in the topo data"},{"average_dip":"(25, 15, 45)","catalog_id":"NEA_259","catalog_name":"GEM_NE_Asia","dip_dir":"S","slip_type":"Reverse","reference":"DEM","epistemic_quality":"1","accuracy":"50000","activity_confidence":"2","downthrown_side_dir":"N","exposure_quality":"2","notes":"Looks like anticlines in Qa at toe, esp in central/east"},{"average_dip":"(50,35,70)","catalog_id":"NEA_255","catalog_name":"GEM_NE_Asia","dip_dir":"S","slip_type":"Sinistral-Reverse","reference":"DEM","epistemic_quality":"1","accuracy":"50000","activity_confidence":"1","downthrown_side_dir":"N","exposure_quality":"2"},{"average_dip":"(90,50,90)","catalog_id":"NEA_254","catalog_name":"GEM_NE_Asia","dip_dir":"S","slip_type":"Sinistral","reference":"DEM","epistemic_quality":"1","accuracy":"100000","activity_confidence":"1","exposure_quality":"2","notes":"Sinistral(?) section in between two inferred sinistral-oblique segments. Inferred to be more SS because of the lack of relief across the fault."},{"average_dip":"(50,35,90)","catalog_id":"NEA_257","catalog_name":"GEM_NE_Asia","dip_dir":"S","slip_type":"Sinistral-Reverse","reference":"DEM","epistemic_quality":"1","accuracy":"50000","activity_confidence":"1","downthrown_side_dir":"N","exposure_quality":"2","notes":"Reverse-SS focal mechanism at E end of fault consistent with sinistral-reverse slip, as is relief across segment."},{"average_dip":"(55,45,65)","catalog_id":"NEA_256","catalog_name":"GEM_NE_Asia","dip_dir":"NW","slip_type":"Normal","reference":"Jolivet et al 2013","epistemic_quality":"1","accuracy":"50000","activity_confidence":"1","downthrown_side_dir":"NW","exposure_quality":"2"},{"average_dip":"(55,45,65)","catalog_id":"NEA_251","catalog_name":"GEM_NE_Asia","dip_dir":"NW","slip_type":"Normal","reference":"Jolivet et al, 2013","epistemic_quality":"1","accuracy":"50000","activity_confidence":"1","downthrown_side_dir":"NW","exposure_quality":"2"},{"average_dip":"(55,45,65)","catalog_id":"NEA_250","catalog_name":"GEM_NE_Asia","dip_dir":"NW","slip_type":"Normal","reference":"Jolivet et al, 2013","epistemic_quality":"1","accuracy":"50000","activity_confidence":"1","downthrown_side_dir":"NW","exposure_quality":"2"},{"average_dip":"(20,10,35)","catalog_id":"NEA_253","catalog_name":"GEM_NE_Asia","dip_dir":"W","slip_type":"Reverse","reference":"Khozurin, 2004","epistemic_quality":"1","accuracy":"50000","activity_confidence":"1","downthrown_side_dir":"E","exposure_quality":"2"},{"average_dip":"(90,,)","catalog_id":"NEA_252","catalog_name":"GEM_NE_Asia","name":"Upper Pil'tun North","slip_type":"Dextral","reference":"Arefiev et al., 2000 GJI","epistemic_quality":"1","accuracy":"50000","activity_confidence":"1","last_movement":"1995","exposure_quality":"2","notes":"Rupture trace of the 1995 Neftegorsk (Ms 7.6) earthquake. Trace is very unclear in the central and northern part, so the wrong scarps may be mapped. However, the trace is here somewhere."},{"average_dip":"(50,20,80)","catalog_id":"NEA_247","catalog_name":"GEM_NE_Asia","dip_dir":"E","name":"Upper Pil'Tun Fault","slip_type":"Dextral-Reverse","reference":"DEM; Khozurin, 2004; Tsutsumi et al., 2005","epistemic_quality":"1","accuracy":"50000","activity_confidence":"1","downthrown_side_dir":"W","exposure_quality":"1"},{"average_dip":"(50,30,70)","catalog_id":"NEA_246","catalog_name":"GEM_NE_Asia","dip_dir":"W","slip_type":"Dextral-Reverse","reference":"DEM; Khozurin, 2004","epistemic_quality":"1","accuracy":"50000","activity_confidence":"1","downthrown_side_dir":"E","exposure_quality":"1","notes":"Pretty great Q offsets"},{"average_dip":"(90,,)","catalog_id":"NEA_249","catalog_name":"GEM_NE_Asia","slip_type":"Dextral","reference":"DEM; Khozurin, 2004","epistemic_quality":"1","accuracy":"100000","activity_confidence":"2","exposure_quality":"1","notes":"Fault of unknown age and activity, but best option for SIberian/Okhotsk plate boundary at this latitude"},{"average_dip":"(50,30,80)","catalog_id":"NEA_248","catalog_name":"GEM_NE_Asia","dip_dir":"E","slip_type":"Dextral-Reverse","reference":"DEM; Khozurin, 2004","epistemic_quality":"1","accuracy":"100000","activity_confidence":"2","downthrown_side_dir":"W","exposure_quality":"1","notes":"Interpreted transpressional stepover on coastal Dzhugdzhur Range fault"},{"average_dip":"(90,,)","catalog_id":"NEA_243","catalog_name":"GEM_NE_Asia","slip_type":"Dextral","reference":"DEM; Khozurin, 2004","epistemic_quality":"1","accuracy":"70000","activity_confidence":"2","exposure_quality":"1","notes":"Best candidate for Siberian-Okhostk plate boundary at this latitude. Khozurin infers dextral slip."},{"average_dip":"(90,,)","catalog_id":"NEA_242","catalog_name":"GEM_NE_Asia","slip_type":"Dextral","reference":"DEM; Khozurin, 2004","epistemic_quality":"2","accuracy":"100000","activity_confidence":"2","exposure_quality":"1","notes":"some structure here, who knows how old"},{"average_dip":"(45,25,65)","catalog_id":"NEA_245","catalog_name":"GEM_NE_Asia","dip_dir":"E","slip_type":"Reverse","reference":"DEM","epistemic_quality":"1","accuracy":"70000","activity_confidence":"2","downthrown_side_dir":"W","exposure_quality":"2","notes":"Interpreted as an east-dipping reverse fault, given the general plate kinematics at this part of the globe. However, it could be an inactive west-dipping normal fault."},{"average_dip":"(90,,)","catalog_id":"NEA_244","catalog_name":"GEM_NE_Asia","slip_type":"Dextral","reference":"DEM; Kozhurin 2004","epistemic_quality":"1","accuracy":"150000","activity_confidence":"2","exposure_quality":"2","notes":"Long lineament in imagery, google earth. Some seismicity in region, minor velocity gradient."},{"average_dip":"(90,,)","catalog_id":"NEA_239","catalog_name":"GEM_NE_Asia","slip_type":"Dextral","reference":"DEM; Khozurin, 2004","epistemic_quality":"1","accuracy":"150000","activity_confidence":"2","exposure_quality":"2","notes":"Old fault / lineament. Some regional seismicity, velocity gradient."},{"average_dip":"(90,,)","catalog_id":"NEA_238","catalog_name":"GEM_NE_Asia","slip_type":"Dextral","reference":"DEM; Khozurin, 2004","epistemic_quality":"1","accuracy":"150000","activity_confidence":"2","exposure_quality":"2","notes":"Old bedrock fault. May be active. Some regional seismicity, GPS velocity gradient."},{"average_dip":"(90,,)","catalog_id":"NEA_241","catalog_name":"GEM_NE_Asia","name":"Ketanda Fault","slip_type":"Dextral","reference":"Khozurin, 2004","epistemic_quality":"1","accuracy":"150000","activity_confidence":"1","strike_slip_rate":"(0.5, 0., 5.)","exposure_quality":"1","notes":"Huge apparent slip rate gradient across fault (long distance though, maybe data problems)."},{"average_dip":"(55,45,65)","catalog_id":"NEA_240","catalog_name":"GEM_NE_Asia","dip_dir":"S","slip_type":"Normal","reference":"DEM","epistemic_quality":"1","accuracy":"50000","activity_confidence":"1","downthrown_side_dir":"S","exposure_quality":"1"},{"average_dip":"(55,45,65)","catalog_id":"NEA_235","catalog_name":"GEM_NE_Asia","dip_dir":"S","name":"Chita Fault, western segment","slip_type":"Normal","reference":"DEM, Lunina Faults","epistemic_quality":"1","accuracy":"40000","activity_confidence":"1","downthrown_side_dir":"S","exposure_quality":"1"},{"average_dip":"(55,45,65)","catalog_id":"NEA_234","catalog_name":"GEM_NE_Asia","dip_dir":"S","name":"Chita Fault","slip_type":"Normal","reference":"DEM","epistemic_quality":"1","accuracy":"50000","activity_confidence":"1","downthrown_side_dir":"S","exposure_quality":"1"},{"average_dip":"(55,45,65)","catalog_id":"NEA_237","catalog_name":"GEM_NE_Asia","dip_dir":"S","name":"Ulaan Ude Fault","slip_type":"Normal","reference":"DEM; Lunina Faults","epistemic_quality":"1","accuracy":"50000","activity_confidence":"1","downthrown_side_dir":"S","exposure_quality":"1"},{"average_dip":"(55,45,65)","catalog_id":"NEA_236","catalog_name":"GEM_NE_Asia","dip_dir":"S","slip_type":"Normal","reference":"DEM; Lunina Faults","epistemic_quality":"1","accuracy":"50000","activity_confidence":"1","downthrown_side_dir":"S","exposure_quality":"1"},{"average_dip":"(50,35,70)","average_rake":"","catalog_id":"NAF_0","catalog_name":"GEM_N_Africa","dip_dir":"W","name":"Tazimi Fault","net_slip_rate":"","slip_type":"Normal","reference":"DEM","epistemic_quality":"2","accuracy":"30000","activity_confidence":"2","fs_name":"Kassita Graben","last_movement":"","downthrown_side_dir":"W","vert_sep_rate":"","strike_slip_rate":"","exposure_quality":"2","shortening_rate":"","notes":""},{"average_dip":"(65,50,85)","average_rake":"","catalog_id":"NAF_1","catalog_name":"GEM_N_Africa","dip_dir":"NW","name":"Nekor Fault","net_slip_rate":"","slip_type":"Sinistral-Normal","reference":"DEM; van der Woerd et al., 2014; d'Acremont et al., 2014","epistemic_quality":"2","accuracy":"50000","activity_confidence":"2","fs_name":"Nekor Fault","last_movement":"","downthrown_side_dir":"NW","vert_sep_rate":"","strike_slip_rate":"","exposure_quality":"2","shortening_rate":"","notes":"Hard to see in imagery but evident scarp in slope map from 30m SRTM"},{"average_dip":"(50,35,60)","average_rake":"","catalog_id":"NAF_2","catalog_name":"GEM_N_Africa","dip_dir":"W","name":"Trougout Fault","net_slip_rate":"","slip_type":"Normal-Sinistral","reference":"Poujol et al., 2014 J. Geodyn.","epistemic_quality":"1","accuracy":"50000","activity_confidence":"1","fs_name":"Low-Nekor Graben","last_movement":"","downthrown_side_dir":"W","vert_sep_rate":"(0.82,,)","strike_slip_rate":"(0.5,,)","exposure_quality":"1","shortening_rate":"(-0.12,,)","notes":""},{"average_dip":"(50,40,65)","average_rake":"","catalog_id":"NAF_3","catalog_name":"GEM_N_Africa","dip_dir":"E","name":"Boujibar Fault","net_slip_rate":"","slip_type":"Normal","reference":"Puojol et al., 2014 G. Geodynamics","epistemic_quality":"2","accuracy":"30000","activity_confidence":"2","fs_name":"Low-Nekor Graben","last_movement":"","downthrown_side_dir":"E","vert_sep_rate":"","strike_slip_rate":"","exposure_quality":"1","shortening_rate":"","notes":""},{"average_dip":"(50,40,65)","average_rake":"","catalog_id":"NAF_4","catalog_name":"GEM_N_Africa","dip_dir":"E","name":"Imzouren Fault","net_slip_rate":"","slip_type":"Normal","reference":"Poujol et al., 2014 J. Geodynamics","epistemic_quality":"2","accuracy":"50000","activity_confidence":"2","fs_name":"Low-Nekor Graben","last_movement":"","downthrown_side_dir":"E","vert_sep_rate":"","strike_slip_rate":"","exposure_quality":"2","shortening_rate":"","notes":"May be at the next terrace flight down"},{"average_dip":"(50,40,65)","average_rake":"","catalog_id":"NAF_5","catalog_name":"GEM_N_Africa","dip_dir":"E","name":"Trougout Fault","net_slip_rate":"","slip_type":"Normal-Sinistral","reference":"Poujol et al., 2014 J. Geodynamics","epistemic_quality":"1","accuracy":"50000","activity_confidence":"1","fs_name":"Low-Nekor Graben","last_movement":"","downthrown_side_dir":"E","vert_sep_rate":"","strike_slip_rate":"","exposure_quality":"2","shortening_rate":"","notes":""},{"average_dip":"(45,30,50)","average_rake":"","catalog_id":"NAF_6","catalog_name":"GEM_N_Africa","dip_dir":"N","name":"Amekchoud-Imidir Thrust","net_slip_rate":"","slip_type":"Reverse","reference":"Pastor et al., 2012 Annals of Geophysics","epistemic_quality":"1","accuracy":"65000","activity_confidence":"1","fs_name":"Sub-Atlas Thrust","last_movement":"","downthrown_side_dir":"S","vert_sep_rate":"","strike_slip_rate":"","exposure_quality":"1","shortening_rate":"(0.1, 0.05, 0.15)","notes":""},{"average_dip":"(30,10,35)","average_rake":"","catalog_id":"NAF_7","catalog_name":"GEM_N_Africa","dip_dir":"N","name":"Jebel Guersif Thrust","net_slip_rate":"","slip_type":"Reverse","reference":"Teson et al., 2008 Int. J. Earth Sci.","epistemic_quality":"1","accuracy":"65000","activity_confidence":"2","fs_name":"Sub-Atlas Thrust","last_movement":"","downthrown_side_dir":"S","vert_sep_rate":"","strike_slip_rate":"","exposure_quality":"2","shortening_rate":"(0.1, 0.0, 0.15)","notes":"Thrust breaks through anticline; Teson has another blind thrust ~~200 m south. He also has a steep (~30\u00b0 ramp soling into a 5 flat at sea level."},{"average_dip":"(20,10,30)","average_rake":"","catalog_id":"NAF_8","catalog_name":"GEM_N_Africa","dip_dir":"S","name":"Midelt Thrust","net_slip_rate":"","slip_type":"Reverse","reference":"DEM","epistemic_quality":"2","accuracy":"30000","activity_confidence":"2","fs_name":"","last_movement":"","downthrown_side_dir":"N","vert_sep_rate":"","strike_slip_rate":"","exposure_quality":"2","shortening_rate":"","notes":"Good expression of scarp on DEM."},{"average_dip":"(30,20,40)","average_rake":"","catalog_id":"NAF_9","catalog_name":"GEM_N_Africa","dip_dir":"NW","name":"Ait Oufella Frontal Thrust","net_slip_rate":"","slip_type":"Reverse","reference":"Rigby 2008 M.S. Thesis (Univ. Missouri)","epistemic_quality":"1","accuracy":"30000","activity_confidence":"1","fs_name":"Ait Oufella Thrust","last_movement":"","downthrown_side_dir":"SE","vert_sep_rate":"","strike_slip_rate":"","exposure_quality":"1","shortening_rate":"(0.1, 0.03, 1)","notes":"Balanced X-Sec shows a flat at 1 km above sea level ~5 degree)."},{"average_dip":"(30,20,35)","average_rake":"","catalog_id":"NAF_10","catalog_name":"GEM_N_Africa","dip_dir":"N","name":"Ait Oufella Frontal Thrust","net_slip_rate":"","slip_type":"Reverse","reference":"DEM","epistemic_quality":"1","accuracy":"30000","activity_confidence":"1","fs_name":"Ait Oufella Thrust","last_movement":"","downthrown_side_dir":"S","vert_sep_rate":"","strike_slip_rate":"","exposure_quality":"1","shortening_rate":"","notes":"little transfer structure"},{"average_dip":"(25,15,35)","average_rake":"","catalog_id":"NAF_11","catalog_name":"GEM_N_Africa","dip_dir":"N","name":"Ait Oufella Frontal Thrust","net_slip_rate":"","slip_type":"Reverse","reference":"DEM","epistemic_quality":"1","accuracy":"30000","activity_confidence":"1","fs_name":"Ait Oufella Thrust","last_movement":"","downthrown_side_dir":"S","vert_sep_rate":"","strike_slip_rate":"","exposure_quality":"1","shortening_rate":"","notes":""},{"average_dip":"","average_rake":"","catalog_id":"NAF_12","catalog_name":"GEM_N_Africa","dip_dir":"","name":"","net_slip_rate":"","slip_type":"Anticline","reference":"DEM, Google Earth","epistemic_quality":"2","accuracy":"30000","activity_confidence":"2","fs_name":"","last_movement":"","downthrown_side_dir":"","vert_sep_rate":"","strike_slip_rate":"","exposure_quality":"2","shortening_rate":"","notes":""},{"average_dip":"(75,60,90)","average_rake":"","catalog_id":"NAF_13","catalog_name":"GEM_N_Africa","dip_dir":"NW","name":"El Ksabi Fault","net_slip_rate":"","slip_type":"Sinistral-Reverse","reference":"DEM; Gomez et al. 1996 J. Geo. Soc. London","epistemic_quality":"2","accuracy":"30000","activity_confidence":"1","fs_name":"","last_movement":"","downthrown_side_dir":"SE","vert_sep_rate":"","strike_slip_rate":"","exposure_quality":"2","shortening_rate":"","notes":""},{"average_dip":"","average_rake":"","catalog_id":"NAF_14","catalog_name":"GEM_N_Africa","dip_dir":"N","name":"South Middle Atlas Frontal Thrust","net_slip_rate":"","slip_type":"Blind Thrust","reference":"DEM","epistemic_quality":"2","accuracy":"60000","activity_confidence":"1","fs_name":"","last_movement":"","downthrown_side_dir":"S","vert_sep_rate":"","strike_slip_rate":"","exposure_quality":"2","shortening_rate":"","notes":"Blind thrust; anticline is very well exposed. Likely merges with South Middle Atlas Thrust at depth."},{"average_dip":"(20,15,60)","average_rake":"","catalog_id":"NAF_15","catalog_name":"GEM_N_Africa","dip_dir":"SE","name":"Beni-Mellal Fault","net_slip_rate":"","slip_type":"Reverse","reference":"Arboleya et al., 2004 JAES","epistemic_quality":"2","accuracy":"30000","activity_confidence":"2","fs_name":"","last_movement":"","downthrown_side_dir":"NW","vert_sep_rate":"","strike_slip_rate":"","exposure_quality":"2","shortening_rate":"","notes":"Lithologic boundary that likely corresponds to older rift-bounding normal fault. Could be steep, could be shallow. "},{"average_dip":"(25,10,40)","average_rake":"","catalog_id":"NAF_16","catalog_name":"GEM_N_Africa","dip_dir":"S","name":"Tigheboula Thrust","net_slip_rate":"","slip_type":"Reverse","reference":"Arboleya et al., 2004 JAES","epistemic_quality":"1","accuracy":"60000","activity_confidence":"1","fs_name":"","last_movement":"","downthrown_side_dir":"N","vert_sep_rate":"","strike_slip_rate":"","exposure_quality":"1","shortening_rate":"","notes":"frontal nappe-bounding thrust to main Beni-Mellal thrust"},{"average_dip":"(30,14,50)","average_rake":"","catalog_id":"NAF_17","catalog_name":"GEM_N_Africa","dip_dir":"NW","name":"South Middle Atlas Rangefront Thrust","net_slip_rate":"","slip_type":"Reverse","reference":"Pastor et al., 2015 Tectonophysics","epistemic_quality":"1","accuracy":"30000","activity_confidence":"2","fs_name":"","last_movement":"","downthrown_side_dir":"SE","vert_sep_rate":"","strike_slip_rate":"","exposure_quality":"1","shortening_rate":"","notes":"Rangefront thrust; may not be currently active, but basinward blind thrusts probably sole in at ~1 km depth or so. May be steep reactivated rift-bounding normal fault, or may be shallower thrust."},{"average_dip":"(15,5,30)","average_rake":"","catalog_id":"NAF_18","catalog_name":"GEM_N_Africa","dip_dir":"NW","name":"South Middle Atlas Frontal Thrust","net_slip_rate":"","slip_type":"Reverse","reference":"DEM","epistemic_quality":"1","accuracy":"30000","activity_confidence":"1","fs_name":"","last_movement":"","downthrown_side_dir":"SE","vert_sep_rate":"","strike_slip_rate":"","exposure_quality":"2","shortening_rate":"","notes":"Blind thrust and anticline. "},{"average_dip":"(10,5,30)","average_rake":"","catalog_id":"NAF_19","catalog_name":"GEM_N_Africa","dip_dir":"NW","name":"","net_slip_rate":"","slip_type":"Reverse","reference":"DEM","epistemic_quality":"2","accuracy":"60000","activity_confidence":"2","fs_name":"","last_movement":"","downthrown_side_dir":"SE","vert_sep_rate":"","strike_slip_rate":"","exposure_quality":"2","shortening_rate":"","notes":"Possible blind thrust in basin."},{"average_dip":"","average_rake":"","catalog_id":"NAF_20","catalog_name":"GEM_N_Africa","dip_dir":"","name":"Tsouaint-Arhal-Tamdafelt Anticline","net_slip_rate":"","slip_type":"Anticline","reference":"Laville et al., 2007 Int. J. Earth Sci., Pastor et al., 2015 Tectonophysics","epistemic_quality":"1","accuracy":"60000","activity_confidence":"2","fs_name":"","last_movement":"","downthrown_side_dir":"","vert_sep_rate":"","strike_slip_rate":"","exposure_quality":"1","shortening_rate":"","notes":""},{"average_dip":"(20,15,60)","average_rake":"(90,,)","catalog_id":"NAF_21","catalog_name":"GEM_N_Africa","dip_dir":"N","name":"Kasbah Thrust","net_slip_rate":"None","slip_type":"Reverse","reference":"1998 GSL","epistemic_quality":"2","accuracy":"70000","activity_confidence":"2","fs_name":"South Atlas Fault","last_movement":"1960","downthrown_side_dir":"S","vert_sep_rate":"","strike_slip_rate":"","exposure_quality":"2","shortening_rate":"","notes":"Some surface rupturing during the 1960 Agadir earthqake, which may or may not have been on a ramp of this fault at depth to the north."},{"average_dip":"(20,15,50)","average_rake":"","catalog_id":"NAF_22","catalog_name":"GEM_N_Africa","dip_dir":"N","name":"South Atlas Thrust","net_slip_rate":"","slip_type":"Reverse","reference":"Sebrier et al., 2006 Geodynamics","epistemic_quality":"2","accuracy":"50000","activity_confidence":"2","fs_name":"South Atlas Thrust","last_movement":"","downthrown_side_dir":"S","vert_sep_rate":"","strike_slip_rate":"","exposure_quality":"2","shortening_rate":"(0.1,,)","notes":"Blind?"},{"average_dip":"(20,15,40)","average_rake":"","catalog_id":"NAF_23","catalog_name":"GEM_N_Africa","dip_dir":"N","name":"South Atlas Thrust","net_slip_rate":"","slip_type":"Reverse","reference":"Sebrier et al., 2006 Geodynamics","epistemic_quality":"2","accuracy":"70000","activity_confidence":"2","fs_name":"South Atlas Thrust","last_movement":"","downthrown_side_dir":"S","vert_sep_rate":"","strike_slip_rate":"","exposure_quality":"2","shortening_rate":"None","notes":"No clear rupture but some possibilities. Also some evidence of folding/ blind thrusting into the basin."},{"average_dip":"(15,15,30)","average_rake":"","catalog_id":"NAF_24","catalog_name":"GEM_N_Africa","dip_dir":"S","name":"","net_slip_rate":"","slip_type":"Reverse","reference":"DEM","epistemic_quality":"2","accuracy":"70000","activity_confidence":"2","fs_name":"North Atlas Thrust","last_movement":"","downthrown_side_dir":"N","vert_sep_rate":"","strike_slip_rate":"","exposure_quality":"1","shortening_rate":"","notes":"Spotted on DEM and Google Earth. "},{"average_dip":"(25,15,40)","average_rake":"","catalog_id":"NAF_25","catalog_name":"GEM_N_Africa","dip_dir":"S","name":"North Atlas Fault","net_slip_rate":"","slip_type":"Reverse","reference":"Sebrier et al., 2006 Geodynamics","epistemic_quality":"2","accuracy":"70000","activity_confidence":"2","fs_name":"North Atlas Fault","last_movement":"","downthrown_side_dir":"N","vert_sep_rate":"","strike_slip_rate":"","exposure_quality":"2","shortening_rate":"","notes":"Rangefront fault, mostly (some deformed rocks to north). No idea if it's active or where the trace is, mapped mostly from DEM."},{"average_dip":"(15,10,30)","average_rake":"","catalog_id":"NAF_26","catalog_name":"GEM_N_Africa","dip_dir":"S","name":"","net_slip_rate":"","slip_type":"Reverse","reference":"DEM","epistemic_quality":"2","accuracy":"70000","activity_confidence":"2","fs_name":"North Atlas Fault","last_movement":"","downthrown_side_dir":"N","vert_sep_rate":"","strike_slip_rate":"","exposure_quality":"2","shortening_rate":"","notes":"Front of uplifted fan basinward of the North Atlas Fault.  Looks more active than rangefront fault but this is a tricky orogen."},{"average_dip":"(15,5,30)","average_rake":"","catalog_id":"NAF_27","catalog_name":"GEM_N_Africa","dip_dir":"S","name":"North Atlas Fault","net_slip_rate":"","slip_type":"Reverse","reference":"DEM","epistemic_quality":"2","accuracy":"100000","activity_confidence":"2","fs_name":"North Atlas Fault","last_movement":"","downthrown_side_dir":"N","vert_sep_rate":"","strike_slip_rate":"","exposure_quality":"1","shortening_rate":"","notes":"Strange triangular bedrock salient at North Atlas rangefront. Possibly a nappe."},{"average_dip":"(80,55,90)","average_rake":"","catalog_id":"NAF_28","catalog_name":"GEM_N_Africa","dip_dir":"N","name":"Nekor Fault","net_slip_rate":"(1., 0.1, 2.)","slip_type":"Sinistral","reference":"Poujol et al., 2014 J. Geodynamics","epistemic_quality":"2","accuracy":"70000","activity_confidence":"1","fs_name":"Nekor Fault","last_movement":"","downthrown_side_dir":"S","vert_sep_rate":"","strike_slip_rate":"","exposure_quality":"2","shortening_rate":"","notes":"sinistral-normal in NE, sinistral-reverse in SW"},{"average_dip":"(35,15,70)","average_rake":"","catalog_id":"NAF_29","catalog_name":"GEM_N_Africa","dip_dir":"N","name":"Fez Fault","net_slip_rate":"(1., 0.1, 2.)","slip_type":"Reverse-Sinistral","reference":"DEM, drawn approx. on many maps","epistemic_quality":"2","accuracy":"70000","activity_confidence":"1","fs_name":"Fez Fault","last_movement":"","downthrown_side_dir":"S","vert_sep_rate":"","strike_slip_rate":"","exposure_quality":"2","shortening_rate":"","notes":"Signs of active deformation and GPS gradient at approx. location of frontal thrust of the Rif belt. The Rif structures look very thin-skinned, however, some of the structures observed in the DEM look to be strike-slip. Things are unclear."},{"average_dip":"(70,30,90)","average_rake":"","catalog_id":"NAF_30","catalog_name":"GEM_N_Africa","dip_dir":"N","name":"","net_slip_rate":"","slip_type":"Sinistral-Reverse","reference":"DEM","epistemic_quality":"2","accuracy":"70000","activity_confidence":"2","fs_name":"Rif Thrust","last_movement":"","downthrown_side_dir":"S","vert_sep_rate":"","strike_slip_rate":"","exposure_quality":"2","shortening_rate":"","notes":"Possible trace observed by linking geomorphic features on DEM. Essentially at the southern Rif thrust front, but may not be reactivating old thrust. Some GPS velocity gradient. City of Fez is at western end, should be a primary target of field investigation."},{"average_dip":"(90.0,,)","average_rake":"","catalog_id":"NAF_31","catalog_name":"GEM_N_Africa","dip_dir":"","name":"Sanhaja Fault","net_slip_rate":"","slip_type":"Sinistral","reference":"DEM","epistemic_quality":"2","accuracy":"60000","activity_confidence":"2","fs_name":"Sanhaja Fault","last_movement":"","downthrown_side_dir":"","vert_sep_rate":"","strike_slip_rate":"(0.1, 0., 0.5)","exposure_quality":"1","shortening_rate":"","notes":"Very well expressed lineament in DEM; worth investigation"},{"average_dip":"(20,10,40)","average_rake":"","catalog_id":"NAF_32","catalog_name":"GEM_N_Africa","dip_dir":"N","name":"","net_slip_rate":"","slip_type":"Reverse","reference":"DEM","epistemic_quality":"2","accuracy":"60000","activity_confidence":"1","fs_name":"","last_movement":"","downthrown_side_dir":"S","vert_sep_rate":"","strike_slip_rate":"","exposure_quality":"2","shortening_rate":"(0.1, 0.01, 0.2)","notes":""},{"average_dip":"(20,10,30)","average_rake":"","catalog_id":"NAF_33","catalog_name":"GEM_N_Africa","dip_dir":"N","name":"","net_slip_rate":"","slip_type":"Reverse","reference":"DEM","epistemic_quality":"2","accuracy":"60000","activity_confidence":"2","fs_name":"","last_movement":"","downthrown_side_dir":"S","vert_sep_rate":"","strike_slip_rate":"","exposure_quality":"2","shortening_rate":"(0.1, 0., 0.2)","notes":""},{"average_dip":"(32,25,40)","average_rake":"","catalog_id":"NAF_34","catalog_name":"GEM_N_Africa","dip_dir":"N","name":"","net_slip_rate":"","slip_type":"Reverse","reference":"Belabbes et al., 2009 J. Seismol","epistemic_quality":"1","accuracy":"150000","activity_confidence":"1","fs_name":"","last_movement":"1999","downthrown_side_dir":"S","vert_sep_rate":"","strike_slip_rate":"","exposure_quality":"2","shortening_rate":"(0.1, 0.01, 0.2)","notes":"Hosted the 1999 Ain Temouchent earthquake; good InSAR study."},{"average_dip":"","average_rake":"","catalog_id":"NAF_35","catalog_name":"GEM_N_Africa","dip_dir":"","name":"Oran Anticline","net_slip_rate":"","slip_type":"Anticline","reference":"DEM","epistemic_quality":"1","accuracy":"200000","activity_confidence":"1","fs_name":"","last_movement":"","downthrown_side_dir":"","vert_sep_rate":"","strike_slip_rate":"","exposure_quality":"1","shortening_rate":"","notes":""},{"average_dip":"","average_rake":"","catalog_id":"NAF_36","catalog_name":"GEM_N_Africa","dip_dir":"","name":"","net_slip_rate":"","slip_type":"Anticline","reference":"","epistemic_quality":"0","accuracy":"150000","activity_confidence":"1","fs_name":"","last_movement":"","downthrown_side_dir":"","vert_sep_rate":"","strike_slip_rate":"","exposure_quality":"0","shortening_rate":"","notes":""},{"average_dip":"(20,10,35)","average_rake":"","catalog_id":"NAF_37","catalog_name":"GEM_N_Africa","dip_dir":"S","name":"","net_slip_rate":"","slip_type":"Reverse","reference":"DEM","epistemic_quality":"2","accuracy":"60000","activity_confidence":"2","fs_name":"","last_movement":"","downthrown_side_dir":"N","vert_sep_rate":"","strike_slip_rate":"","exposure_quality":"1","shortening_rate":"","notes":"Looks like an active thrust w/ a rapidly-subsiding hanging-wall basin. No clear scarps but the HW is so smooth and there are no fans so it looks like the HW is dropping fast."},{"average_dip":"(20,10,35)","average_rake":"","catalog_id":"NAF_38","catalog_name":"GEM_N_Africa","dip_dir":"S","name":"Mohammadia Thrust","net_slip_rate":"","slip_type":"Reverse","reference":"DEM","epistemic_quality":"2","accuracy":"50000","activity_confidence":"1","fs_name":"","last_movement":"","downthrown_side_dir":"N","vert_sep_rate":"","strike_slip_rate":"","exposure_quality":"1","shortening_rate":"(0.2, 0., 1.)","notes":"Some signs of warping of Quaternary seds at rangefront, but otherwise looks like  a thrust w/ a rapidly-subsiding foreland. Links up w/ other thrusts and folds (blind thrusts) in many places."},{"average_dip":"(15,5,30)","average_rake":"","catalog_id":"NAF_39","catalog_name":"GEM_N_Africa","dip_dir":"S","name":"","net_slip_rate":"","slip_type":"Reverse","reference":"DEM","epistemic_quality":"1","accuracy":"60000","activity_confidence":"1","fs_name":"","last_movement":"","downthrown_side_dir":"N","vert_sep_rate":"","strike_slip_rate":"","exposure_quality":"1","shortening_rate":"","notes":""},{"average_dip":"(25,10,50)","average_rake":"","catalog_id":"NAF_40","catalog_name":"GEM_N_Africa","dip_dir":"N","name":"","net_slip_rate":"","slip_type":"Reverse","reference":"DEM","epistemic_quality":"1","accuracy":"50000","activity_confidence":"1","fs_name":"","last_movement":"","downthrown_side_dir":"S","vert_sep_rate":"","strike_slip_rate":"","exposure_quality":"1","shortening_rate":"","notes":""},{"average_dip":"(20,10,60)","average_rake":"","catalog_id":"NAF_41","catalog_name":"GEM_N_Africa","dip_dir":"N","name":"Murdjadjo Thrust","net_slip_rate":"","slip_type":"Reverse","reference":"Bouhadad 2001 J. Seismology","epistemic_quality":"1","accuracy":"60000","activity_confidence":"1","fs_name":"","last_movement":"1790?","downthrown_side_dir":"S","vert_sep_rate":"","strike_slip_rate":"","exposure_quality":"1","shortening_rate":"(0.2., 0.01, 1.)","notes":"Bouhadad located field exposures w/ 60 degree dip. This may not characterize the whole structure."},{"average_dip":"(25,10,60)","average_rake":"(90.,45.,90.)","catalog_id":"NAF_42","catalog_name":"GEM_N_Africa","dip_dir":"NW","name":"Bou Kadir Fault","net_slip_rate":"","slip_type":"Reverse","reference":"Aifa and Idres, 2010 Open Geology Journal","epistemic_quality":"1","accuracy":"50000","activity_confidence":"1","fs_name":"","last_movement":"","downthrown_side_dir":"SE","vert_sep_rate":"","strike_slip_rate":"","exposure_quality":"1","shortening_rate":"None","notes":"Possible sinistral component"},{"average_dip":"(20,10,50)","average_rake":"","catalog_id":"NAF_43","catalog_name":"GEM_N_Africa","dip_dir":"N","name":"","net_slip_rate":"","slip_type":"Reverse","reference":"Maouche et al., 2011 Tectonophysics","epistemic_quality":"2","accuracy":"50000","activity_confidence":"2","fs_name":"","last_movement":"","downthrown_side_dir":"S","vert_sep_rate":"","strike_slip_rate":"","exposure_quality":"2","shortening_rate":"","notes":""},{"average_dip":"(40,30,50)","average_rake":"","catalog_id":"NAF_44","catalog_name":"GEM_N_Africa","dip_dir":"NW","name":"El Asnam Fault","net_slip_rate":"","slip_type":"Reverse","reference":"Meghroui et al., 1988 EPSL","epistemic_quality":"1","accuracy":"30000","activity_confidence":"1","fs_name":"El Asnam Fault","last_movement":"1980","downthrown_side_dir":"SE","vert_sep_rate":"(0.6, 0.5, 1.)","strike_slip_rate":"","exposure_quality":"1","shortening_rate":"","notes":"Ruptured in the M7.1-7.3 El Asnam Earthquake"},{"average_dip":"(30,20,60)","average_rake":"","catalog_id":"NAF_45","catalog_name":"GEM_N_Africa","dip_dir":"NW","name":"","net_slip_rate":"","slip_type":"Reverse","reference":"DEM","epistemic_quality":"1","accuracy":"30000","activity_confidence":"1","fs_name":"","last_movement":"","downthrown_side_dir":"SE","vert_sep_rate":"","strike_slip_rate":"","exposure_quality":"1","shortening_rate":"","notes":"Possible fresh scarp at base (visible in 30m DEM)"},{"average_dip":"(30,20,60)","average_rake":"(90,150,10)","catalog_id":"NAF_46","catalog_name":"GEM_N_Africa","dip_dir":"N","name":"","net_slip_rate":"","slip_type":"Reverse","reference":"DEM","epistemic_quality":"2","accuracy":"60000","activity_confidence":"2","fs_name":"","last_movement":"","downthrown_side_dir":"S","vert_sep_rate":"","strike_slip_rate":"","exposure_quality":"1","shortening_rate":"","notes":"Looks like a reverse or oblique-reverse thrust. Not sure of what strike-slip direction, but it's oblique to other thrusts. Could be either based on stress/convergence directions. Basin looks like it's subsiding relatively rapidly but otherwise not a lot of evidence for recent faulting."},{"average_dip":"(20,10,55)","average_rake":"","catalog_id":"NAF_47","catalog_name":"GEM_N_Africa","dip_dir":"N","name":"Sahel Thrust","net_slip_rate":"","slip_type":"Reverse","reference":"Maouche et al., 2011 Tectonophysics","epistemic_quality":"1","accuracy":"30000","activity_confidence":"1","fs_name":"","last_movement":"","downthrown_side_dir":"S","vert_sep_rate":"(1., 0.84, 1.2)","strike_slip_rate":"","exposure_quality":"1","shortening_rate":"","notes":"Rupture traces visible in DEM east of big canyon in middle. Apparent left-lateral offset of drainages across the fault."},{"average_dip":"(20,10,60)","average_rake":"","catalog_id":"NAF_48","catalog_name":"GEM_N_Africa","dip_dir":"S","name":"","net_slip_rate":"","slip_type":"Reverse","reference":"Maouche et al., 2011 Tectonophysics","epistemic_quality":"1","accuracy":"30000","activity_confidence":"1","fs_name":"","last_movement":"","downthrown_side_dir":"N","vert_sep_rate":"","strike_slip_rate":"","exposure_quality":"1","shortening_rate":"","notes":""},{"average_dip":"(35,20,60)","average_rake":"","catalog_id":"NAF_49","catalog_name":"GEM_N_Africa","dip_dir":"S","name":"Mitidja Thrust","net_slip_rate":"","slip_type":"Reverse","reference":"Mouache et al., 2011 Tectonophysics","epistemic_quality":"0","accuracy":"50000","activity_confidence":"1","fs_name":"Mitidja Thrust","last_movement":"","downthrown_side_dir":"N","vert_sep_rate":"","strike_slip_rate":"","exposure_quality":"0","shortening_rate":"","notes":""},{"average_dip":"(35,20,50)","average_rake":"","catalog_id":"NAF_50","catalog_name":"GEM_N_Africa","dip_dir":"S","name":"Mitidja Thrust","net_slip_rate":"","slip_type":"Reverse","reference":"Mouache et al., 2003","epistemic_quality":"1","accuracy":"200000","activity_confidence":"1","fs_name":"Mitidja Thrust","last_movement":"2003","downthrown_side_dir":"N","vert_sep_rate":"","strike_slip_rate":"","exposure_quality":"2","shortening_rate":"","notes":"Ruptured in the 2003 Zemmouri earthquake (M6.8), 0.5 m slip."},{"average_dip":"(55,30,80)","average_rake":"","catalog_id":"NAF_51","catalog_name":"GEM_N_Africa","dip_dir":"N","name":"","net_slip_rate":"","slip_type":"Dextral-Reverse","reference":"DEM","epistemic_quality":"2","accuracy":"100000","activity_confidence":"2","fs_name":"","last_movement":"","downthrown_side_dir":"S","vert_sep_rate":"","strike_slip_rate":"","exposure_quality":"2","shortening_rate":"","notes":"Consistent pattern of right-offset stream drainages. Looks like a dextral fault that swings around into a thrust. The high topo in hanging wall may not be coincidental."},{"average_dip":"(90,,)","average_rake":"","catalog_id":"NAF_52","catalog_name":"GEM_N_Africa","dip_dir":"","name":"Thenia Fault","net_slip_rate":"","slip_type":"Dextral","reference":"Boudiaf et al., 1998 Terra Nova","epistemic_quality":"2","accuracy":"50000","activity_confidence":"2","fs_name":"","last_movement":"","downthrown_side_dir":"","vert_sep_rate":"","strike_slip_rate":"","exposure_quality":"2","shortening_rate":"","notes":""},{"average_dip":"(65,45,89)","average_rake":"","catalog_id":"NAF_53","catalog_name":"GEM_N_Africa","dip_dir":"N","name":"","net_slip_rate":"","slip_type":"Dextral","reference":"Said et al., 2011 Tectonophysics","epistemic_quality":"1","accuracy":"50000","activity_confidence":"1","fs_name":"Gafsa 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Fault","last_movement":"","downthrown_side_dir":"N","vert_sep_rate":"","strike_slip_rate":"","exposure_quality":"2","shortening_rate":"","notes":""},{"average_dip":"(40,20,70)","average_rake":"","catalog_id":"NAF_56","catalog_name":"GEM_N_Africa","dip_dir":"S","name":"Berda Thrust","net_slip_rate":"","slip_type":"Reverse","reference":"Said et al., 2011","epistemic_quality":"2","accuracy":"50000","activity_confidence":"1","fs_name":"","last_movement":"","downthrown_side_dir":"N","vert_sep_rate":"","strike_slip_rate":"","exposure_quality":"2","shortening_rate":"None","notes":"Blind"},{"average_dip":"(30,10,65)","average_rake":"","catalog_id":"NAF_57","catalog_name":"GEM_N_Africa","dip_dir":"N","name":"Orbata Thrust","net_slip_rate":"","slip_type":"Reverse","reference":"Said et al., 2011","epistemic_quality":"1","accuracy":"50000","activity_confidence":"1","fs_name":"Gafsa 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0.2)","notes":""},{"average_dip":"(20,10,50)","average_rake":"","catalog_id":"NAF_61","catalog_name":"GEM_N_Africa","dip_dir":"N","name":"","net_slip_rate":"","slip_type":"Reverse","reference":"DEM","epistemic_quality":"1","accuracy":"30000","activity_confidence":"2","fs_name":"","last_movement":"","downthrown_side_dir":"S","vert_sep_rate":"","strike_slip_rate":"","exposure_quality":"1","shortening_rate":"(0.1, 0.01, 0.2)","notes":""},{"average_dip":"(20,10,50)","average_rake":"","catalog_id":"NAF_62","catalog_name":"GEM_N_Africa","dip_dir":"N","name":"","net_slip_rate":"","slip_type":"Reverse","reference":"DEM","epistemic_quality":"2","accuracy":"20000","activity_confidence":"2","fs_name":"","last_movement":"","downthrown_side_dir":"S","vert_sep_rate":"","strike_slip_rate":"","exposure_quality":"1","shortening_rate":"(0.1, 0.001, 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0.2)","notes":""},{"average_dip":"(20,15,50)","average_rake":"","catalog_id":"NAF_65","catalog_name":"GEM_N_Africa","dip_dir":"N","name":"","net_slip_rate":"","slip_type":"Reverse","reference":"DEM","epistemic_quality":"2","accuracy":"50000","activity_confidence":"2","fs_name":"","last_movement":"","downthrown_side_dir":"S","vert_sep_rate":"","strike_slip_rate":"","exposure_quality":"1","shortening_rate":"(0.1, 0.01, 1)","notes":""},{"average_dip":"(20,10,50)","average_rake":"","catalog_id":"NAF_66","catalog_name":"GEM_N_Africa","dip_dir":"N","name":"","net_slip_rate":"","slip_type":"Reverse","reference":"DEM","epistemic_quality":"1","accuracy":"50000","activity_confidence":"2","fs_name":"South Atlas Front","last_movement":"","downthrown_side_dir":"S","vert_sep_rate":"","strike_slip_rate":"","exposure_quality":"2","shortening_rate":"(0.1, 0.01, 1)","notes":""},{"average_dip":"(20,10,50)","average_rake":"","catalog_id":"NAF_67","catalog_name":"GEM_N_Africa","dip_dir":"N","name":"","net_slip_rate":"","slip_type":"Reverse","reference":"DEM","epistemic_quality":"1","accuracy":"50000","activity_confidence":"1","fs_name":"South Atlas Front","last_movement":"","downthrown_side_dir":"S","vert_sep_rate":"","strike_slip_rate":"","exposure_quality":"1","shortening_rate":"(0.1, 0.01, 1.)","notes":""},{"average_dip":"(20,10,50)","average_rake":"","catalog_id":"NAF_68","catalog_name":"GEM_N_Africa","dip_dir":"N","name":"","net_slip_rate":"","slip_type":"Reverse","reference":"DEM","epistemic_quality":"1","accuracy":"50000","activity_confidence":"2","fs_name":"","last_movement":"","downthrown_side_dir":"S","vert_sep_rate":"","strike_slip_rate":"","exposure_quality":"1","shortening_rate":"","notes":""},{"average_dip":"(20,10,50)","average_rake":"","catalog_id":"NAF_69","catalog_name":"GEM_N_Africa","dip_dir":"N","name":"","net_slip_rate":"","slip_type":"Reverse","reference":"DEM","epistemic_quality":"1","accuracy":"30000","activity_confidence":"2","fs_name":"","last_movement":"","downthrown_side_dir":"S","vert_sep_rate":"","strike_slip_rate":"","exposure_quality":"1","shortening_rate":"","notes":"Unclear if it's active; geomorphically distinct but not evidence HW subsidence.  Some EQs in area."},{"average_dip":"(35,15,60)","average_rake":"","catalog_id":"NAF_70","catalog_name":"GEM_N_Africa","dip_dir":"N","name":"Soummam Fault","net_slip_rate":"","slip_type":"Reverse","reference":"Machane and Bensalem 2015","epistemic_quality":"1","accuracy":"50000","activity_confidence":"1","fs_name":"","last_movement":"","downthrown_side_dir":"S","vert_sep_rate":"","strike_slip_rate":"","exposure_quality":"1","shortening_rate":"","notes":"Minor Quaternary offset observed in field (by Machane and Bensalem), though it's hard to tell tectonic scarps from fluvial features in DEM"},{"average_dip":"(50,20,80)","average_rake":"","catalog_id":"NAF_71","catalog_name":"GEM_N_Africa","dip_dir":"N","name":"Kherrata Fault","net_slip_rate":"","slip_type":"Dextral-Reverse","reference":"Harbi et al., 1999 J. Seismology","epistemic_quality":"2","accuracy":"50000","activity_confidence":"2","fs_name":"Kherrata Fault","last_movement":"","downthrown_side_dir":"S","vert_sep_rate":"","strike_slip_rate":"","exposure_quality":"2","shortening_rate":"","notes":"Very unclear where the active Kherrata Fault is in particular (clearly there are many in the vicinity), to what degree any of them are active, or their rates and kinematics. Nonetheless it's referenced a bit and there is seismicity in the region."},{"average_dip":"(90,,)","average_rake":"","catalog_id":"NAF_72","catalog_name":"GEM_N_Africa","dip_dir":"","name":"","net_slip_rate":"","slip_type":"Dextral","reference":"","epistemic_quality":"2","accuracy":"50000","activity_confidence":"2","fs_name":"Guelma Fault","last_movement":"","downthrown_side_dir":"","vert_sep_rate":"","strike_slip_rate":"","exposure_quality":"2","shortening_rate":"","notes":"Shown in general on lots of maps. Precise location uncertain, activity uncertain, etc..."},{"average_dip":"(90,,)","average_rake":"","catalog_id":"NAF_73","catalog_name":"GEM_N_Africa","dip_dir":"","name":"","net_slip_rate":"","slip_type":"Dextral","reference":"","epistemic_quality":"2","accuracy":"100000","activity_confidence":"2","fs_name":"Guelma Fault","last_movement":"","downthrown_side_dir":"","vert_sep_rate":"","strike_slip_rate":"","exposure_quality":"2","shortening_rate":"","notes":"Shown on lots of maps, with general DEM expression (but no clear fault trace). No idea if it's active, although there is distributed local strike-slip seismicity consistent with dextral slip on a structure like this."},{"average_dip":"(90,,)","average_rake":"","catalog_id":"NAF_74","catalog_name":"GEM_N_Africa","dip_dir":"","name":"Guelma Fault","net_slip_rate":"","slip_type":"Dextral","reference":"","epistemic_quality":"2","accuracy":"150000","activity_confidence":"2","fs_name":"Guelma Fault","last_movement":"","downthrown_side_dir":"","vert_sep_rate":"","strike_slip_rate":"","exposure_quality":"2","shortening_rate":"","notes":"Shown on lots of maps, but actual fault trace (or existence of active faulting) is very unclear."},{"average_dip":"(50,40,70)","average_rake":"","catalog_id":"NAF_75","catalog_name":"GEM_N_Africa","dip_dir":"SW","name":"","net_slip_rate":"","slip_type":"Normal","reference":"DEM","epistemic_quality":"1","accuracy":"30000","activity_confidence":"1","fs_name":"Tebessa Graben","last_movement":"","downthrown_side_dir":"SW","vert_sep_rate":"","strike_slip_rate":"","exposure_quality":"1","shortening_rate":"","notes":"Best-expressed normal fault in the Atlas. Dextral-normal faulting in graben."},{"average_dip":"(50,40,60)","average_rake":"","catalog_id":"NAF_76","catalog_name":"GEM_N_Africa","dip_dir":"NE","name":"Tebessa Fault","net_slip_rate":"","slip_type":"Dextral-Normal","reference":"DEM","epistemic_quality":"1","accuracy":"50000","activity_confidence":"1","fs_name":"Tebessa Graben","last_movement":"","downthrown_side_dir":"NE","vert_sep_rate":"","strike_slip_rate":"","exposure_quality":"1","shortening_rate":"","notes":"5.4 EQ on fault in 1995"},{"average_dip":"(50,40,60)","average_rake":"","catalog_id":"NAF_77","catalog_name":"GEM_N_Africa","dip_dir":"SW","name":"Khmouda Fault","net_slip_rate":"","slip_type":"Normal","reference":"DEM","epistemic_quality":"2","accuracy":"50000","activity_confidence":"1","fs_name":"Kasserine Graben","last_movement":"","downthrown_side_dir":"SW","vert_sep_rate":"","strike_slip_rate":"","exposure_quality":"1","shortening_rate":"","notes":"Neogene? graben. Looks active, but slow."},{"average_dip":"(50,40,60)","average_rake":"","catalog_id":"NAF_78","catalog_name":"GEM_N_Africa","dip_dir":"NE","name":"Jebel Ech Chambi Fault","net_slip_rate":"","slip_type":"Normal","reference":"DEM","epistemic_quality":"1","accuracy":"30000","activity_confidence":"1","fs_name":"Kasserine Graben","last_movement":"","downthrown_side_dir":"NE","vert_sep_rate":"","strike_slip_rate":"","exposure_quality":"1","shortening_rate":"","notes":""},{"average_dip":"(50,40,80)","average_rake":"","catalog_id":"NAF_79","catalog_name":"GEM_N_Africa","dip_dir":"N","name":"Kasserine Fault","net_slip_rate":"","slip_type":"Dextral-Normal","reference":"DEM","epistemic_quality":"1","accuracy":"50000","activity_confidence":"1","fs_name":"Kasserine Graben","last_movement":"","downthrown_side_dir":"N","vert_sep_rate":"","strike_slip_rate":"","exposure_quality":"1","shortening_rate":"","notes":""},{"average_dip":"(50,40,70)","average_rake":"","catalog_id":"NAF_80","catalog_name":"GEM_N_Africa","dip_dir":"NE","name":"","net_slip_rate":"","slip_type":"Dextral-Normal","reference":"DEM","epistemic_quality":"2","accuracy":"50000","activity_confidence":"2","fs_name":"Kasserine Graben","last_movement":"","downthrown_side_dir":"NE","vert_sep_rate":"","strike_slip_rate":"","exposure_quality":"2","shortening_rate":"","notes":""},{"average_dip":"(70,50,90)","average_rake":"","catalog_id":"NAF_81","catalog_name":"GEM_N_Africa","dip_dir":"S","name":"","net_slip_rate":"","slip_type":"Dextral","reference":"DEM","epistemic_quality":"1","accuracy":"50000","activity_confidence":"1","fs_name":"","last_movement":"","downthrown_side_dir":"S","vert_sep_rate":"","strike_slip_rate":"","exposure_quality":"1","shortening_rate":"","notes":"good geomorphic expression. Possibly some normal fault (down to the south) slip as well."},{"average_dip":"(50,40,70)","average_rake":"","catalog_id":"NAF_82","catalog_name":"GEM_N_Africa","dip_dir":"W","name":"","net_slip_rate":"","slip_type":"Normal","reference":"DEM","epistemic_quality":"2","accuracy":"30000","activity_confidence":"2","fs_name":"Sabibah Graben","last_movement":"","downthrown_side_dir":"W","vert_sep_rate":"","strike_slip_rate":"","exposure_quality":"2","shortening_rate":"","notes":""},{"average_dip":"(50,40,70)","average_rake":"","catalog_id":"NAF_83","catalog_name":"GEM_N_Africa","dip_dir":"E","name":"","net_slip_rate":"","slip_type":"Normal","reference":"DEM","epistemic_quality":"2","accuracy":"70000","activity_confidence":"2","fs_name":"Sabibah Graben","last_movement":"","downthrown_side_dir":"E","vert_sep_rate":"","strike_slip_rate":"","exposure_quality":"2","shortening_rate":"","notes":"Maybe active... Was certainly active in Neogene, but Quaternary activity uncertain."},{"average_dip":"(50,30,70)","average_rake":"","catalog_id":"NAF_84","catalog_name":"GEM_N_Africa","dip_dir":"W","name":"N-S Axial Fault","net_slip_rate":"","slip_type":"Sinistral-Reverse","reference":"Soumaya et al., 2015 Tectonics","epistemic_quality":"1","accuracy":"200000","activity_confidence":"1","fs_name":"N-S Axial Fault","last_movement":"","downthrown_side_dir":"E","vert_sep_rate":"","strike_slip_rate":"","exposure_quality":"2","shortening_rate":"","notes":"Blind oblique-reverse (?) fault under major regional fold. A fair amount of associated seismicity, but it looks like an inverted (or reactivated) basement structure.  It's in a lot of papers but no good surface break."},{"average_dip":"(60,40,80)","average_rake":"","catalog_id":"NAF_85","catalog_name":"GEM_N_Africa","dip_dir":"W","name":"N-S Axial Fault","net_slip_rate":"","slip_type":"Sinistral-Reverse","reference":"Soumaya et al., 2015","epistemic_quality":"1","accuracy":"250000","activity_confidence":"1","fs_name":"N-S Axial Fault","last_movement":"","downthrown_side_dir":"E","vert_sep_rate":"","strike_slip_rate":"","exposure_quality":"2","shortening_rate":"","notes":"Blind reverse-oblique (?) fault below well-defined anticline. Lots of associated moderate seismicity but kinematics and geometry a little unclear."},{"average_dip":"(50.0,,)","average_rake":"","catalog_id":"NAF_86","catalog_name":"GEM_N_Africa","dip_dir":"E","name":"Western Fault","net_slip_rate":"","slip_type":"Normal","reference":"Abdunasser and McCaffrey 2015 J. 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JAES","epistemic_quality":"1","accuracy":"64000","activity_confidence":"1","fs_name":"","last_movement":"","downthrown_side_dir":"","vert_sep_rate":"","strike_slip_rate":"","exposure_quality":"1","shortening_rate":"","notes":""},{"average_dip":"(55,40,70)","average_rake":"","catalog_id":"NAF_93","catalog_name":"GEM_N_Africa","dip_dir":"W","name":"Nezzazat Fault","net_slip_rate":"","slip_type":"Normal","reference":"Sharp et al. 2000 GSAB","epistemic_quality":"1","accuracy":"100000","activity_confidence":"1","fs_name":"","last_movement":"","downthrown_side_dir":"W","vert_sep_rate":"","strike_slip_rate":"","exposure_quality":"1","shortening_rate":"","notes":""},{"average_dip":"(60,40,80)","average_rake":"","catalog_id":"NAF_94","catalog_name":"GEM_N_Africa","dip_dir":"S","name":"Markha Baba transfer Fault","net_slip_rate":"","slip_type":"Normal","reference":"Sharp et al. 2000","epistemic_quality":"1","accuracy":"20000","activity_confidence":"1","fs_name":"","last_movement":"","downthrown_side_dir":"S","vert_sep_rate":"","strike_slip_rate":"","exposure_quality":"1","shortening_rate":"","notes":"May be oblique"},{"average_dip":"(60,40,70)","average_rake":"","catalog_id":"NAF_95","catalog_name":"GEM_N_Africa","dip_dir":"W","name":"Hadahid Fault","net_slip_rate":"","slip_type":"Normal","reference":"Sharp et al. 2000","epistemic_quality":"1","accuracy":"40000","activity_confidence":"1","fs_name":"","last_movement":"","downthrown_side_dir":"W","vert_sep_rate":"","strike_slip_rate":"","exposure_quality":"1","shortening_rate":"","notes":""},{"average_dip":"(60,40,70)","average_rake":"","catalog_id":"NAF_96","catalog_name":"GEM_N_Africa","dip_dir":"W","name":"Sinai Massif Fault","net_slip_rate":"","slip_type":"Normal","reference":"Sharp et al. 2000","epistemic_quality":"1","accuracy":"50000","activity_confidence":"1","fs_name":"","last_movement":"","downthrown_side_dir":"W","vert_sep_rate":"","strike_slip_rate":"","exposure_quality":"1","shortening_rate":"","notes":""},{"average_dip":"(50,40,70)","average_rake":"","catalog_id":"NAF_97","catalog_name":"GEM_N_Africa","dip_dir":"W","name":"South Sinai Massif Fault","net_slip_rate":"","slip_type":"Normal","reference":"DEM","epistemic_quality":"1","accuracy":"150000","activity_confidence":"1","fs_name":"","last_movement":"","downthrown_side_dir":"W","vert_sep_rate":"","strike_slip_rate":"","exposure_quality":"1","shortening_rate":"","notes":""},{"average_dip":"(55,40,70)","average_rake":"","catalog_id":"NAF_98","catalog_name":"GEM_N_Africa","dip_dir":"W","name":"","net_slip_rate":"","slip_type":"Normal","reference":"DEM","epistemic_quality":"1","accuracy":"100000","activity_confidence":"2","fs_name":"","last_movement":"","downthrown_side_dir":"W","vert_sep_rate":"","strike_slip_rate":"","exposure_quality":"1","shortening_rate":"","notes":"Gets a little ambiguous towards the north and south. Might not be very active."},{"average_dip":"(60,40,70)","average_rake":"","catalog_id":"NAF_99","catalog_name":"GEM_N_Africa","dip_dir":"N","name":"St. Anthony Fault","net_slip_rate":"","slip_type":"Normal","reference":"DEM","epistemic_quality":"1","accuracy":"100000","activity_confidence":"1","fs_name":"","last_movement":"","downthrown_side_dir":"N","vert_sep_rate":"","strike_slip_rate":"","exposure_quality":"1","shortening_rate":"","notes":"Some scarps in Google Earth. Strange structure."},{"average_dip":"(60,40,70)","average_rake":"","catalog_id":"NAF_100","catalog_name":"GEM_N_Africa","dip_dir":"S","name":"","net_slip_rate":"","slip_type":"Normal","reference":"DEM","epistemic_quality":"1","accuracy":"70000","activity_confidence":"2","fs_name":"","last_movement":"","downthrown_side_dir":"S","vert_sep_rate":"","strike_slip_rate":"","exposure_quality":"1","shortening_rate":"","notes":"Can't find any real scarps in Google Earth but could be marginally active"},{"average_dip":"(50,40,70)","average_rake":"","catalog_id":"NAF_101","catalog_name":"GEM_N_Africa","dip_dir":"N","name":"","net_slip_rate":"","slip_type":"Normal","reference":"DEM","epistemic_quality":"1","accuracy":"30000","activity_confidence":"1","fs_name":"","last_movement":"","downthrown_side_dir":"N","vert_sep_rate":"","strike_slip_rate":"","exposure_quality":"1","shortening_rate":"","notes":""},{"average_dip":"(60,40,70)","average_rake":"","catalog_id":"NAF_102","catalog_name":"GEM_N_Africa","dip_dir":"N","name":"","net_slip_rate":"","slip_type":"Normal","reference":"DEM","epistemic_quality":"1","accuracy":"50000","activity_confidence":"1","fs_name":"","last_movement":"","downthrown_side_dir":"N","vert_sep_rate":"","strike_slip_rate":"","exposure_quality":"1","shortening_rate":"","notes":"Gorgeous tectonic geomorphology in DEM and Google 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in bathymetry "},{"average_dip":"(90,60,90)","average_rake":"(0.,0.,45.)","catalog_id":"NAF_115","catalog_name":"GEM_N_Africa","dip_dir":"S","name":"","net_slip_rate":"","slip_type":"Sinistral","reference":"DEM; seismicity","epistemic_quality":"1","accuracy":"500000","activity_confidence":"1","fs_name":"","last_movement":"2016","downthrown_side_dir":"N","vert_sep_rate":"","strike_slip_rate":"(0.5, 0.1, 1.5)","exposure_quality":"2","shortening_rate":"","notes":"Mw 6.4 on 2016-01-25 in GCMT catalog"},{"average_dip":"(90,,)","average_rake":"(180,,)","catalog_id":"NAF_116","catalog_name":"GEM_N_Africa","dip_dir":"","name":"Yusuf Fault","net_slip_rate":"","slip_type":"Dextral","reference":"Mauffret et al. 2017","epistemic_quality":"1","accuracy":"500000","activity_confidence":"1","fs_name":"","last_movement":"","downthrown_side_dir":"","vert_sep_rate":"","strike_slip_rate":"(1.5, 0.5, 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thrusts."},{"average_dip":"(30,20,60)","average_rake":"(90.,90.,135)","catalog_id":"NAF_124","catalog_name":"GEM_N_Africa","dip_dir":"S","name":"","net_slip_rate":"(0.5,0.1,1.)","slip_type":"Reverse","reference":"Bathymetry, Mauffret 2007","epistemic_quality":"2","accuracy":"500000","activity_confidence":"2","fs_name":"","last_movement":"","downthrown_side_dir":"N","vert_sep_rate":"","strike_slip_rate":"","exposure_quality":"2","shortening_rate":"","notes":"poorly drawn w/ wrong strike-slip kinematics in Mauffret, based on newer data"},{"average_dip":"(30,20,50)","average_rake":"(90,90,135)","catalog_id":"NAF_125","catalog_name":"GEM_N_Africa","dip_dir":"S","name":"","net_slip_rate":"(0.5,0.1,1.)","slip_type":"Reverse","reference":"DEM","epistemic_quality":"2","accuracy":"500000","activity_confidence":"1","fs_name":"","last_movement":"","downthrown_side_dir":"N","vert_sep_rate":"","strike_slip_rate":"","exposure_quality":"2","shortening_rate":"","notes":"May have been responsible for 2003 Bourmedes EQ or some aftershocks"},{"average_dip":"(30,20,50)","average_rake":"(90.,90.,135.)","catalog_id":"NAF_126","catalog_name":"GEM_N_Africa","dip_dir":"S","name":"","net_slip_rate":"(1.5,0.5,2.5)","slip_type":"Reverse","reference":"Bathymetry; Mauffret 2007","epistemic_quality":"2","accuracy":"500000","activity_confidence":"2","fs_name":"","last_movement":"","downthrown_side_dir":"N","vert_sep_rate":"","strike_slip_rate":"","exposure_quality":"2","shortening_rate":"","notes":"Another likely offshore reverse fault with possible dextral slip"},{"average_dip":"(70,70,90)","average_rake":"(180,135,180)","catalog_id":"NAF_127","catalog_name":"GEM_N_Africa","dip_dir":"W","name":"","net_slip_rate":"(1.5,0.5,2.5)","slip_type":"Dextral","reference":"Bathymetry; focal mechs; Mauffret 2007","epistemic_quality":"2","accuracy":"500000","activity_confidence":"1","fs_name":"","last_movement":"","downthrown_side_dir":"E","vert_sep_rate":"","strike_slip_rate":"","exposure_quality":"2","shortening_rate":"","notes":""},{"average_dip":"(30,20,50)","average_rake":"(90,90,135)","catalog_id":"NAF_128","catalog_name":"GEM_N_Africa","dip_dir":"S","name":"","net_slip_rate":"(1.5,0.5,2.5)","slip_type":"Reverse","reference":"Bathymetry; Mauffret 2007","epistemic_quality":"2","accuracy":"400000","activity_confidence":"2","fs_name":"","last_movement":"","downthrown_side_dir":"N","vert_sep_rate":"","strike_slip_rate":"","exposure_quality":"2","shortening_rate":"","notes":""},{"average_dip":"(30,20,50)","average_rake":"(90.,90.,135.)","catalog_id":"NAF_129","catalog_name":"GEM_N_Africa","dip_dir":"S","name":"","net_slip_rate":"(1.5,0.5,2.5)","slip_type":"Reverse","reference":"Bathymetry; Mauffret 2007","epistemic_quality":"2","accuracy":"500000","activity_confidence":"2","fs_name":"","last_movement":"","downthrown_side_dir":"N","vert_sep_rate":"","strike_slip_rate":"","exposure_quality":"2","shortening_rate":"","notes":""},{"average_dip":"(30,20,50)","average_rake":"(90.,90.,135.)","catalog_id":"NAF_130","catalog_name":"GEM_N_Africa","dip_dir":"S","name":"","net_slip_rate":"(1.5,0.5,2.5)","slip_type":"Reverse","reference":"Bathymetry; Mauffret 2007","epistemic_quality":"2","accuracy":"500000","activity_confidence":"2","fs_name":"","last_movement":"","downthrown_side_dir":"N","vert_sep_rate":"","strike_slip_rate":"","exposure_quality":"2","shortening_rate":"","notes":""},{"average_dip":"(45,20,60)","average_rake":"","catalog_id":"NAF_131","catalog_name":"GEM_N_Africa","dip_dir":"N","name":"","net_slip_rate":"","slip_type":"Reverse-Dextral","reference":"DEM","epistemic_quality":"2","accuracy":"0","activity_confidence":"2","fs_name":"","last_movement":"","downthrown_side_dir":"S","vert_sep_rate":"","strike_slip_rate":"","exposure_quality":"2","shortening_rate":"","notes":"Doesn't look active as nearby traces but fills in a deformation gap and there is a basin (maybe old?)"},{"average_dip":"(20,10,30)","average_rake":"(90,,)","catalog_id":"NAF_132","catalog_name":"GEM_N_Africa","dip_dir":"E","name":"","net_slip_rate":"(0.75,0.25,1.5)","slip_type":"Reverse","reference":"DEM","epistemic_quality":"2","accuracy":"60000","activity_confidence":"2","fs_name":"","last_movement":"","downthrown_side_dir":"W","vert_sep_rate":"","strike_slip_rate":"","exposure_quality":"2","shortening_rate":"","notes":"westernmost Rif thrust. It's got to be somewhere and this is a convenient topographic escarpemnt."},{"average_dip":"(20,10,30)","average_rake":"(90,,)","catalog_id":"NAF_133","catalog_name":"GEM_N_Africa","dip_dir":"E","name":"","net_slip_rate":"(0.75,0.25,1.5)","slip_type":"Reverse","reference":"DEM","epistemic_quality":"2","accuracy":"100000","activity_confidence":"2","fs_name":"Rif thrusts","last_movement":"","downthrown_side_dir":"W","vert_sep_rate":"","strike_slip_rate":"","exposure_quality":"2","shortening_rate":"","notes":"Westernmost Rif thrust; hard to place trace exactly but seismicity and GPS stop here"},{"average_dip":"(20,10,30)","average_rake":"(90.,,)","catalog_id":"NAF_134","catalog_name":"GEM_N_Africa","dip_dir":"E","name":"","net_slip_rate":"(1.,0.5,2.)","slip_type":"Reverse","reference":"DEM; Koulali et al., 2011","epistemic_quality":"2","accuracy":"150000","activity_confidence":"1","fs_name":"","last_movement":"","downthrown_side_dir":"W","vert_sep_rate":"","strike_slip_rate":"","exposure_quality":"2","shortening_rate":"","notes":"Koulali has it mapped (from earlier sources?) but does not draw a GPS block boundary along it. Nonetheless there  is a ~1mm/yr velocity gradient across it."},{"average_dip":"(90,,)","average_rake":"","catalog_id":"NAF_135","catalog_name":"GEM_N_Africa","dip_dir":"","name":"Kalabsha Fault","net_slip_rate":"","slip_type":"Strike-Slip","reference":"DEM; Mekkawi et al., 2005 EPSL; Kebeasy et al., 1987","epistemic_quality":"1","accuracy":"30000","activity_confidence":"1","fs_name":"","last_movement":"","downthrown_side_dir":"","vert_sep_rate":"","strike_slip_rate":"","exposure_quality":"1","shortening_rate":"","notes":"Basement structure that shows mild deformation of Cenozoic sediments above. Thought by Kebeasy to be the host of teh 1981 Aswan earthquake; those papers are unavailable to me but they found evidence fro ground deformation. The Aswan earthquake is widely believed to be from elevated stresses and fluid pressure following the filling of Lake Nasser."},{"average_dip":"(75,60,90)","catalog_id":"CA_1.0","catalog_name":"GEM_Central_Am_Carib","dip_dir":"S","name":"Tuxtla Fault","net_slip_rate":"(6.,4.,8.)","slip_type":"Sinistral","reference":"Witt et al., 2012","epistemic_quality":"1","accuracy":"100000","activity_confidence":"1","fs_name":"Tuxtla-Malpaso Fault Zone","vert_sep_rate":"(0,,)","exposure_quality":"1"},{"average_dip":"(90,60,90)","catalog_id":"CA_2.0","catalog_name":"GEM_Central_Am_Carib","name":"Malpaso Fault","net_slip_rate":"(2.,0.,2.)","slip_type":"Sinistral","reference":"Witt et al., 2012","epistemic_quality":"1","accuracy":"100000","activity_confidence":"1","fs_name":"Tuxtla-Malpaso Fault Zone","exposure_quality":"1"},{"average_dip":"(90,,)","catalog_id":"CA_3.0","catalog_name":"GEM_Central_Am_Carib","name":"San Cristobal 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BSSA"},{"catalog_id":"CA_164.0","catalog_name":"GEM_Central_Am_Carib","dip_dir":"S","name":"North Caribbean Megathrust (North Hispaniola Fault)","net_slip_rate":"(2.5,1.5,3.5)","slip_type":"Reverse-Sinistral","reference":"Symithe et al., 2015","activity_confidence":"1","downthrown_side_dir":"N","notes":""},{"catalog_id":"CA_165.0","catalog_name":"GEM_Central_Am_Carib","dip_dir":"S","name":"North Cuban Fault","slip_type":"Reverse","reference":"Garcia et al., 2003 BSSA","accuracy":"500000"},{"catalog_id":"CA_166.0","catalog_name":"GEM_Central_Am_Carib","dip_dir":"W","name":"Cay Sal Fault","slip_type":"Reverse","reference":"Kula, 2014 U. Miami MS Thesis","accuracy":"500000","activity_confidence":"1","downthrown_side_dir":"E"},{"catalog_id":"CA_167.0","catalog_name":"GEM_Central_Am_Carib","name":"Septentrional Fault","slip_type":"Sinistral","accuracy":"200000","activity_confidence":"1","fs_name":"Septentrional Fault"},{"catalog_id":"CA_168.0","catalog_name":"GEM_Central_Am_Carib","dip_dir":"E","name":"West Mona Rift Fault","slip_type":"Normal","activity_confidence":"1","fs_name":"Mona Rift","downthrown_side_dir":"E","shortening_rate":"None"},{"catalog_id":"CA_169.0","catalog_name":"GEM_Central_Am_Carib","dip_dir":"W","name":"East Mona Rift Fault","slip_type":"Normal","accuracy":"500000","activity_confidence":"1","downthrown_side_dir":"W","shortening_rate":"None"},{"catalog_id":"CA_170.0","catalog_name":"GEM_Central_Am_Carib","dip_dir":"E","name":"West Yuma Rift Fault","slip_type":"Normal","reference":"Hippolyte et al., 2005 GSA SP; Symithe et al., 2015","fs_name":"Yuma Rift","downthrown_side_dir":"E","shortening_rate":"None"},{"catalog_id":"CA_171.0","catalog_name":"GEM_Central_Am_Carib","dip_dir":"W","name":"East Yuma Rift Fault","slip_type":"Normal","reference":"Hippolyte et al., 2005 GSA SP; Symithe et al., 2015","fs_name":"Yuma Rift","downthrown_side_dir":"W","shortening_rate":"None"},{"catalog_id":"CA_172.0","catalog_name":"GEM_Central_Am_Carib","dip_dir":"NE","slip_type":"Reverse","reference":"Benford et al., 2012 GJI","activity_confidence":"1","fs_name":"Muertos Thrust","downthrown_side_dir":"SW"},{"catalog_id":"CA_173.0","catalog_name":"GEM_Central_Am_Carib","dip_dir":"N","name":"Muertos Thrust","slip_type":"Reverse","activity_confidence":"1","fs_name":"Muertos Thrust","downthrown_side_dir":"S"},{"catalog_id":"CA_174.0","catalog_name":"GEM_Central_Am_Carib","dip_dir":"N","slip_type":"Normal","reference":"Mann et al., 2005 GSA SP","fs_name":"Anegada Rift","downthrown_side_dir":"N"},{"catalog_id":"CA_175.0","catalog_name":"GEM_Central_Am_Carib","dip_dir":"N","name":"St. Croix Fault","slip_type":"Normal","reference":"Mann et al., 2005 GSA SP","fs_name":"Anegada Rift","downthrown_side_dir":"N"},{"catalog_id":"CA_176.0","catalog_name":"GEM_Central_Am_Carib","dip_dir":"S","name":"Sombrero Fault","slip_type":"Normal","reference":"Mann et al., 2005 GSA SP","fs_name":"Anegada Rift","downthrown_side_dir":"S"},{"catalog_id":"CA_177.0","catalog_name":"GEM_Central_Am_Carib","name":"Enriquillo-Plantain Garden Fault","slip_type":"Sinistral_Transform","activity_confidence":"1","fs_name":"Enriquillo-Plantain Garden Fault"},{"catalog_id":"CA_178.0","catalog_name":"GEM_Central_Am_Carib","name":"Oriente Fault","slip_type":"Sinistral_Transform","reference":"Leroy et al., 2015 Terra Nova","epistemic_quality":"1","accuracy":"500000","activity_confidence":"1","fs_name":"Oriente Fault Zone","exposure_quality":"2"},{"catalog_id":"CA_179.0","catalog_name":"GEM_Central_Am_Carib","dip_dir":"N","name":"Santiago Deformed Belt","slip_type":"Reverse","reference":"Leroy et al., 2015 Terra Nova","epistemic_quality":"2","activity_confidence":"2","fs_name":"Oriente Fault","downthrown_side_dir":"S","exposure_quality":"2"},{"catalog_id":"CA_180.0","catalog_name":"GEM_Central_Am_Carib","name":"Oriente Fault","slip_type":"Sinistral_Transform","reference":"Leroy et al., 2015 Terra Nova","epistemic_quality":"1","accuracy":"500000","activity_confidence":"1","fs_name":"Oriente Fault Zone"},{"catalog_id":"CA_181.0","catalog_name":"GEM_Central_Am_Carib","name":"Walton Fault Zone","slip_type":"Sinistral_Transform","reference":"Leroy et al., 2015 Terra Nova","accuracy":"1000000","activity_confidence":"1","fs_name":"Walton Fault Zone","strike_slip_rate":"None","notes":"Slip rates from residual from total relative plate motion - Oriente Fault"},{"catalog_id":"CA_182.0","catalog_name":"GEM_Central_Am_Carib","name":"Swan Islands Transform","slip_type":"Sinistral_Transform","reference":"Rogers and Mann, 2007","epistemic_quality":"1","accuracy":"1000000","activity_confidence":"1","fs_name":"Swan Islands Transform","strike_slip_rate":"None"},{"catalog_id":"CA_261.0","catalog_name":"GEM_Central_Am_Carib","name":"Swan Islands Transform","slip_type":"Sinistral_Transform","reference":"Rogers and Mann, 2007","epistemic_quality":"1","accuracy":"1000000","activity_confidence":"1","fs_name":"Swan Islands Transform","strike_slip_rate":"None"},{"catalog_id":"CA_184.0","catalog_name":"GEM_Central_Am_Carib","name":"Cayman Spreading Center","slip_type":"Spreading_Ridge","reference":"Leroy et al., 2000; Hayman et al., 2011","epistemic_quality":"1","accuracy":"1000000","activity_confidence":"1","exposure_quality":"1","shortening_rate":"(-13,-16,-10)","notes":"Likely thin seismogenic thickness, may not produce moderate to large earthquakes. "},{"catalog_id":"CA_186.0","catalog_name":"GEM_Central_Am_Carib","dip_dir":"W","name":"Antilles Thrust","slip_type":"Reverse","epistemic_quality":"1","activity_confidence":"1","downthrown_side_dir":"E"},{"average_dip":"(20,10,50)","average_rake":"(90,,)","catalog_id":"CA_187.0","catalog_name":"GEM_Central_Am_Carib","dip_dir":"E","name":"Middle America Trench megathrust","slip_type":"Subduction_Thrust","epistemic_quality":"1","accuracy":"1000000","activity_confidence":"1","fs_name":"Middle America Trench","downthrown_side_dir":"W","exposure_quality":"1","shortening_rate":"(75,50,90)"},{"average_dip":"(90,,)","catalog_id":"CA_188.0","catalog_name":"GEM_Central_Am_Carib","name":"Falla Canoas","slip_type":"Dextral","reference":"Camacho 2003 Tecnociencia","epistemic_quality":"1","accuracy":"50000","activity_confidence":"1","exposure_quality":"2"},{"average_dip":"(90,,)","catalog_id":"CA_189.0","catalog_name":"GEM_Central_Am_Carib","name":"Zona Falla Media","slip_type":"Dextral","reference":"Camacho 2003 Tecnociencia","epistemic_quality":"1","accuracy":"60000","activity_confidence":"1","exposure_quality":"2"},{"catalog_id":"CA_190.0","catalog_name":"GEM_Central_Am_Carib","name":"Falla Longitudinal-Boca Chica","reference":"Camacho 2003 Tectnociencia","accuracy":"60000","activity_confidence":"1"},{"average_dip":"(90,,)","catalog_id":"CA_191.0","catalog_name":"GEM_Central_Am_Carib","slip_type":"Sinistral","reference":"Camacho 2003 Tecnociencia","accuracy":"100000"},{"average_dip":"(90,,)","catalog_id":"CA_192.0","catalog_name":"GEM_Central_Am_Carib","name":"Azuero Fault","slip_type":"Sinistral","reference":"Rockwell et al. 2010 Tectonics","accuracy":"60000","activity_confidence":"1","strike_slip_rate":"None","notes":"GPS predicts 9 \u00b1 2 mm/yr of extension, but this is  not at all evident in the geology."},{"average_dip":"(90,,)","catalog_id":"CA_193.0","catalog_name":"GEM_Central_Am_Carib","name":"Azuero Fault","slip_type":"Sinistral","reference":"DEM, Rockwell 2010 Tectonics","epistemic_quality":"2","accuracy":"30000","activity_confidence":"1","downthrown_side_dir":"N","exposure_quality":"2"},{"average_dip":"(90,,)","catalog_id":"CA_194.0","catalog_name":"GEM_Central_Am_Carib","name":"Azuero Fault","slip_type":"Sinistral","reference":"DEM, Rockwell et al., 2010","accuracy":"100000","activity_confidence":"1","downthrown_side_dir":"N","strike_slip_rate":"None"},{"average_dip":"(80,50,90)","catalog_id":"CA_195.0","catalog_name":"GEM_Central_Am_Carib","dip_dir":"N","net_slip_rate":"(1,0.1,3)","slip_type":"Sinistral-Normal","reference":"DEM","accuracy":"70000","activity_confidence":"1","fs_name":"Azuero Fault Zone","downthrown_side_dir":"N","notes":"Topographically well expressed in a rapidly-eroding tropical region.  Looks more normal in E, more sinsitral in W."},{"average_dip":"(90,,)","catalog_id":"CA_196.0","catalog_name":"GEM_Central_Am_Carib","name":"Rincon Hondo Fault","slip_type":"Sinistral","reference":"DEM","epistemic_quality":"2","accuracy":"70000","activity_confidence":"2","exposure_quality":"1","notes":"Interesting expression in DEM. Unclear if it's active but given the inferred kinematics and lack of similar topographic lineaments in the area, it probably is."},{"average_dip":"(80,70,90)","catalog_id":"CA_197.0","catalog_name":"GEM_Central_Am_Carib","dip_dir":"E","reference":"DEM","epistemic_quality":"2","accuracy":"75000","activity_confidence":"2","downthrown_side_dir":"E","exposure_quality":"2","notes":"Very distinct escarpment in DEM. Unclear of age or activity."},{"average_dip":"(80,70,90)","catalog_id":"CA_198.0","catalog_name":"GEM_Central_Am_Carib","dip_dir":"E","reference":"DEM","epistemic_quality":"2","accuracy":"60000","activity_confidence":"2","downthrown_side_dir":"E","exposure_quality":"1","notes":"Looks like a transtensional fault, bounding the west side of a graben."},{"average_dip":"(90,,)","catalog_id":"CA_199.0","catalog_name":"GEM_Central_Am_Carib","name":"Rio Gatun Fault","slip_type":"Sinistral","reference":"Rockwell et al. 2010","epistemic_quality":"1","accuracy":"150000","activity_confidence":"1","strike_slip_rate":"None","notes":"Rate based on a regional GPS model that may ovrestimate slip rate on individual faults."},{"average_dip":"(80,70,90)","catalog_id":"CA_200.0","catalog_name":"GEM_Central_Am_Carib","dip_dir":"E","name":"Limon Fault","slip_type":"Dextral-Normal","reference":"Bennett et al., 2014 SRL","epistemic_quality":"2","accuracy":"150000","activity_confidence":"1","downthrown_side_dir":"E","strike_slip_rate":"None","shortening_rate":"None"},{"catalog_id":"CA_203.0","catalog_name":"GEM_Central_Am_Carib","dip_dir":"S","name":"North Caribbean Megathrust","slip_type":"Reverse","activity_confidence":"1","downthrown_side_dir":"N"},{"average_dip":"(70,50,90)","catalog_id":"CA_204.0","catalog_name":"GEM_Central_Am_Carib","dip_dir":"S","slip_type":"Sinistral","reference":"Grindlay et al. 2005","epistemic_quality":"2","accuracy":"300000","activity_confidence":"1","fs_name":"Bunce Fault Zone","exposure_quality":"2"},{"average_dip":"(60,50,70)","catalog_id":"CA_205.0","catalog_name":"GEM_Central_Am_Carib","dip_dir":"W","slip_type":"Normal-Sinistral","reference":"DEM; Grindlay et al. 2005","epistemic_quality":"2","accuracy":"200000","activity_confidence":"2","fs_name":"Bunce Fault Zone","downthrown_side_dir":"W","exposure_quality":"1","notes":"Appears to be a transtensional segment of the Bunce Fault Zone in the bathymetry.."},{"average_dip":"(60,50,70)","catalog_id":"CA_206.0","catalog_name":"GEM_Central_Am_Carib","dip_dir":"E","slip_type":"Sinistral-Normal","reference":"Bathymetry; Grindlay et al. 2005","epistemic_quality":"2","accuracy":"200000","activity_confidence":"2","fs_name":"Bunce Fault Zone","downthrown_side_dir":"E","exposure_quality":"1"},{"average_dip":"(90,70,90)","catalog_id":"CA_207.0","catalog_name":"GEM_Central_Am_Carib","dip_dir":"S","name":"Bunce Fault","slip_type":"Sinistral","reference":"Grindlay et al. 2005","epistemic_quality":"2","accuracy":"300000","activity_confidence":"2","fs_name":"Bunce Fault Zone","exposure_quality":"2"},{"average_dip":"(80,70,90)","catalog_id":"CA_208.0","catalog_name":"GEM_Central_Am_Carib","dip_dir":"S","name":"Bunce Fault","slip_type":"Sinistral","reference":"Grindlay et al. 2005","epistemic_quality":"2","accuracy":"300000","activity_confidence":"2","fs_name":"Bunce Fault Zone","exposure_quality":"2","notes":"Soles into the megathrust at shallow depths. May have some reverse component on it.  Really hard to make out in bathymetry."},{"average_dip":"(70,60,90)","catalog_id":"CA_209.0","catalog_name":"GEM_Central_Am_Carib","dip_dir":"S","name":"Bunce Fault","slip_type":"Sinistral","reference":"Grindlay et al. 2005","epistemic_quality":"2","accuracy":"400000","activity_confidence":"2","fs_name":"Bunce Fault Zone","exposure_quality":"2","notes":"Soles into megathrust at shallow depth. May not be seismogenic. Very few constraints on this one..."},{"average_dip":"(90,,)","catalog_id":"CA_210.0","catalog_name":"GEM_Central_Am_Carib","name":"Bowin Fault","slip_type":"Sinistral","reference":"Grindlay et al. 2005","epistemic_quality":"2","accuracy":"300000","activity_confidence":"2","fs_name":"Bowin Fault Zone","exposure_quality":"2"},{"average_dip":"(90,,)","catalog_id":"CA_211.0","catalog_name":"GEM_Central_Am_Carib","name":"Bowin Fault","slip_type":"Sinistral","reference":"Grindlay et al. 2005","epistemic_quality":"2","accuracy":"200000","activity_confidence":"2","fs_name":"Bowin Fault Zon","exposure_quality":"2"},{"average_dip":"(90,,)","catalog_id":"CA_212.0","catalog_name":"GEM_Central_Am_Carib","slip_type":"Sinistral","reference":"Grindlay et al. 2005","epistemic_quality":"2","accuracy":"200000","activity_confidence":"2","fs_name":"Bowin Fault Zone","exposure_quality":"2"},{"average_dip":"(90,,)","catalog_id":"CA_213.0","catalog_name":"GEM_Central_Am_Carib","slip_type":"Sinistral","reference":"Grindlay et al. 2005","accuracy":"300000","activity_confidence":"2","fs_name":"Bowin Fault Zone"},{"average_dip":"(90,,)","catalog_id":"CA_214.0","catalog_name":"GEM_Central_Am_Carib","slip_type":"Sinistral","reference":"Grindlay et al. 2005","epistemic_quality":"2","accuracy":"300000","activity_confidence":"2","fs_name":"Bowin Fault Zone","exposure_quality":"2"},{"average_dip":"(90,,)","catalog_id":"CA_215.0","catalog_name":"GEM_Central_Am_Carib","slip_type":"Sinistral","reference":"Grindlay et al. 2005","epistemic_quality":"2","accuracy":"300000","activity_confidence":"2","fs_name":"Bowin Fault Zone","exposure_quality":"2"},{"average_dip":"(20,10,50)","catalog_id":"CA_216.0","catalog_name":"GEM_Central_Am_Carib","dip_dir":"S","slip_type":"Reverse","reference":"Bathymetry","epistemic_quality":"2","accuracy":"300000","activity_confidence":"2","fs_name":"Bowin Fault Zone","downthrown_side_dir":"N","exposure_quality":"2","notes":"Looks in the bathymetry like a thrust at the base of the Puerto Rican slope. May tie in to the Bowin Fault Zone somehow."},{"average_dip":"(90,,)","catalog_id":"CA_217.0","catalog_name":"GEM_Central_Am_Carib","name":"Bunce Fault","slip_type":"Sinistral","reference":"Grindlay et al. 2005","epistemic_quality":"2","accuracy":"500000","activity_confidence":"2","fs_name":"Bunce Fault Zone","exposure_quality":"2","notes":"May have some reverse component, but information is completely lacking."},{"average_dip":"(90,,)","catalog_id":"CA_218.0","catalog_name":"GEM_Central_Am_Carib","slip_type":"Dextral-Normal","reference":"Jansma and Mattioli 2005","epistemic_quality":"2","accuracy":"80000","activity_confidence":"2","fs_name":"Great Northern Puerto Rico Fault Zone","exposure_quality":"2","notes":"Probably inactive"},{"average_dip":"(90,,)","catalog_id":"CA_219.0","catalog_name":"GEM_Central_Am_Carib","slip_type":"Dextral-Normal","reference":"Jansma and Mattioli 2005","epistemic_quality":"2","accuracy":"80000","activity_confidence":"2","fs_name":"Great Northern Puerto Rico Fault Zone","exposure_quality":"2","notes":"Almost certainly inactive"},{"average_dip":"(90,,)","catalog_id":"CA_220.0","catalog_name":"GEM_Central_Am_Carib","slip_type":"Dextral-Normal","reference":"Jansma and Mattioli 2005","epistemic_quality":"2","accuracy":"100000","activity_confidence":"2","fs_name":"Great Northern Puerto Rico Fault Zone","exposure_quality":"2","notes":"Almost certainly inactive"},{"average_dip":"(90,,)","catalog_id":"CA_221.0","catalog_name":"GEM_Central_Am_Carib","slip_type":"Dextral-Normal","reference":"Jansma and Mattioli 2005","epistemic_quality":"2","accuracy":"80000","activity_confidence":"2","fs_name":"Great Northern Puerto Rico Fault Zone","exposure_quality":"2","notes":"Almost certainly inactive"},{"average_dip":"(70,50,90)","catalog_id":"CA_222.0","catalog_name":"GEM_Central_Am_Carib","dip_dir":"NE","slip_type":"Sinistral-Normal","reference":"Feuillet et al. 2011","epistemic_quality":"2","accuracy":"500000","activity_confidence":"2","downthrown_side_dir":"NE","exposure_quality":"2","notes":"Location not constrained by any topography or bathymetry, only by approximating Fueillet's lines."},{"average_dip":"(70,50,90)","catalog_id":"CA_223.0","catalog_name":"GEM_Central_Am_Carib","dip_dir":"N","slip_type":"Sinistral-Normal","reference":"Feuillet et al. 2011","epistemic_quality":"2","accuracy":"500000","activity_confidence":"2","downthrown_side_dir":"N","exposure_quality":"2","notes":"Approximated from source; no bathymetric signature on available low-resolution imagery."},{"average_dip":"(70,50,90)","catalog_id":"CA_224.0","catalog_name":"GEM_Central_Am_Carib","dip_dir":"NE","slip_type":"Sinistral-Normal","reference":"Feuillet et al., 2011","epistemic_quality":"2","accuracy":"500000","activity_confidence":"2","downthrown_side_dir":"NE","exposure_quality":"2"},{"average_dip":"(60,50,80)","catalog_id":"CA_225.0","catalog_name":"GEM_Central_Am_Carib","dip_dir":"NE","slip_type":"Normal-Sinistral","reference":"Feuillet et al. 2011","epistemic_quality":"2","accuracy":"500000","activity_confidence":"2","downthrown_side_dir":"NE","exposure_quality":"2"},{"average_dip":"(60,50,70)","catalog_id":"CA_226.0","catalog_name":"GEM_Central_Am_Carib","dip_dir":"NE","slip_type":"Normal-Sinistral","reference":"Feuillet et al. 2011","epistemic_quality":"2","accuracy":"500000","downthrown_side_dir":"NE","exposure_quality":"2"},{"average_dip":"(60,50,70)","catalog_id":"CA_227.0","catalog_name":"GEM_Central_Am_Carib","dip_dir":"NE","slip_type":"Sinistral-Normal","reference":"Feuillet et al. 2011","epistemic_quality":"2","accuracy":"500000","activity_confidence":"1","last_movement":"1897","downthrown_side_dir":"NE","exposure_quality":"2"},{"average_dip":"(75,70,80)","catalog_id":"CA_228.0","catalog_name":"GEM_Central_Am_Carib","dip_dir":"N","name":"Morne Piton Fault","slip_type":"Normal","reference":"Feuillet et al 2004","epistemic_quality":"1","accuracy":"500000","activity_confidence":"1","downthrown_side_dir":"N","vert_sep_rate":"(0.5, 0.3, 0.7)","exposure_quality":"2"},{"average_dip":"(60,50,70)","catalog_id":"CA_229.0","catalog_name":"GEM_Central_Am_Carib","dip_dir":"E","slip_type":"Normal","reference":"Feuillet et al 2011","epistemic_quality":"1","accuracy":"500000","activity_confidence":"1","last_movement":"2004","downthrown_side_dir":"E","exposure_quality":"2"},{"average_dip":"(60,50,70)","catalog_id":"CA_230.0","catalog_name":"GEM_Central_Am_Carib","dip_dir":"W","slip_type":"Normal","reference":"Feuillet et al. 2011","epistemic_quality":"2","accuracy":"750000","activity_confidence":"1","last_movement":"1967","downthrown_side_dir":"W","exposure_quality":"2"},{"average_dip":"(60,50,70)","catalog_id":"CA_231.0","catalog_name":"GEM_Central_Am_Carib","dip_dir":"E","slip_type":"Normal","reference":"Feuillet et al. 2004","epistemic_quality":"2","accuracy":"500000","activity_confidence":"2","downthrown_side_dir":"E","exposure_quality":"2"},{"average_dip":"(60,50,70)","catalog_id":"CA_232.0","catalog_name":"GEM_Central_Am_Carib","dip_dir":"W","slip_type":"Normal","reference":"Feuillet et al. 2004","epistemic_quality":"2","accuracy":"500000","activity_confidence":"2","downthrown_side_dir":"W","exposure_quality":"2"},{"average_dip":"(60,50,70)","catalog_id":"CA_233.0","catalog_name":"GEM_Central_Am_Carib","dip_dir":"W","slip_type":"Normal","reference":"Feuillet et al. 2004","epistemic_quality":"2","accuracy":"500000","activity_confidence":"2","downthrown_side_dir":"W","exposure_quality":"2"},{"average_dip":"(60,50,70)","catalog_id":"CA_234.0","catalog_name":"GEM_Central_Am_Carib","dip_dir":"SE","slip_type":"Normal","reference":"Feuillet et al. 2004","epistemic_quality":"2","accuracy":"500000","activity_confidence":"2","downthrown_side_dir":"SE","exposure_quality":"2"},{"average_dip":"(60,50,70)","catalog_id":"CA_235.0","catalog_name":"GEM_Central_Am_Carib","dip_dir":"S","slip_type":"Normal","reference":"Feuillet et al. 2004","epistemic_quality":"2","accuracy":"500000","activity_confidence":"2","last_movement":"1897?","downthrown_side_dir":"S","exposure_quality":"2"},{"average_dip":"(60,50,70)","catalog_id":"CA_236.0","catalog_name":"GEM_Central_Am_Carib","dip_dir":"E","slip_type":"Normal","reference":"Calais and de Lepinay, 1991","accuracy":"700000","activity_confidence":"1","downthrown_side_dir":"E"},{"average_dip":"(60,50,70)","catalog_id":"CA_237.0","catalog_name":"GEM_Central_Am_Carib","dip_dir":"E","slip_type":"Normal","reference":"Calail and de Lepinay, 1991","accuracy":"700000","activity_confidence":"1","downthrown_side_dir":"E"},{"average_dip":"(60,50,70)","catalog_id":"CA_238.0","catalog_name":"GEM_Central_Am_Carib","dip_dir":"E","slip_type":"Normal","reference":"Calais and de Lepinay, 1991","accuracy":"700000","activity_confidence":"1"},{"catalog_id":"CA_239.0","catalog_name":"GEM_Central_Am_Carib","name":"Oriente Fault","slip_type":"Sinistral_Transform","reference":"Leroy et al., 2015 Terra Nova","epistemic_quality":"1","accuracy":"500000","activity_confidence":"1","fs_name":"Oriente Fault Zone"},{"average_dip":"(90,70,90)","catalog_id":"CA_240.0","catalog_name":"GEM_Central_Am_Carib","dip_dir":"E","name":"Pedro Miguel Fault","slip_type":"Dextral","reference":"Rockwell et al., 2010","epistemic_quality":"1","accuracy":"100000","activity_confidence":"1","downthrown_side_dir":"E","strike_slip_rate":"(5.,3.5,8.)","exposure_quality":"1"},{"average_dip":"(90,,)","catalog_id":"CA_241.0","catalog_name":"GEM_Central_Am_Carib","name":"Rio Gatun Fault","slip_type":"Sinistral","reference":"DEM; Rockwell et al., 2010a,b","epistemic_quality":"1","accuracy":"150000","activity_confidence":"1","strike_slip_rate":"None","exposure_quality":"2","notes":"Trace location modified from sources based on DEM"},{"average_dip":"(90,,)","catalog_id":"CA_242.0","catalog_name":"GEM_Central_Am_Carib","name":"Rio Gatun Fault","slip_type":"Sinistral","reference":"DEM; Rockwell et al., 2010a, b","epistemic_quality":"1","accuracy":"75000","activity_confidence":"1","strike_slip_rate":"None","exposure_quality":"1","notes":"Geometry modified from source based on SRTM30 data"},{"catalog_id":"CA_243.0","catalog_name":"GEM_Central_Am_Carib","name":"Rio Gatun Fault","slip_type":"Sinistral","reference":"DEM; Rockwell et al., 2010a,b","epistemic_quality":"2","accuracy":"300000","activity_confidence":"1","strike_slip_rate":"None","exposure_quality":"2","notes":"Interpreted geometry (the whole fault segment is underwater)"},{"average_dip":"(60,40,70)","catalog_id":"CA_244.0","catalog_name":"GEM_Central_Am_Carib","dip_dir":"S","name":"Tela Fault","slip_type":"Normal","reference":"Rogers and Mann, 2007","epistemic_quality":"1","accuracy":"500000","activity_confidence":"1","downthrown_side_dir":"S","exposure_quality":"2","notes":"Good seismic profiles in Rogers and Mann 2007"},{"average_dip":"(90,,)","catalog_id":"CA_245.0","catalog_name":"GEM_Central_Am_Carib","name":"Flowers Bay Fault","slip_type":"Sinistral","reference":"Cox et al., 2008","epistemic_quality":"1","accuracy":"50000","activity_confidence":"1","exposure_quality":"2","notes":"Cox et al. map southwestern offshore portion as normal, but unclear why"},{"average_dip":"(60,40,70)","catalog_id":"CA_246.0","catalog_name":"GEM_Central_Am_Carib","dip_dir":"W","name":"Sebaco Fault","slip_type":"Normal","reference":"DEM","epistemic_quality":"2","accuracy":"35000","activity_confidence":"2","downthrown_side_dir":"W","exposure_quality":"1","notes":"Very clear scarp in topopgraphy data and a hanging-wall basin that looks to be actively subsiding (no erosion despite external drainage, river near fault). Nonetheless, no clear quaternary scarps observed."},{"average_dip":"(75,50,90)","catalog_id":"CA_247.0","catalog_name":"GEM_Central_Am_Carib","dip_dir":"E","name":"Aeropuerto Fault","slip_type":"Sinistral-Reverse","reference":"Cowen et al., 2002","epistemic_quality":"1","accuracy":"100000","activity_confidence":"1","downthrown_side_dir":"E","vert_sep_rate":"(0.6,0.3,0.9)","strike_slip_rate":"None","exposure_quality":"2","notes":"Most rapid slip probably sinistral. Hard to locate trace on DEM."},{"average_dip":"(80,70,90)","catalog_id":"CA_248.0","catalog_name":"GEM_Central_Am_Carib","dip_dir":"E","name":"Tiscapa Fault","slip_type":"Sinistral-Normal","reference":"Freundt et al., 2010; Brown et al., 1973","epistemic_quality":"1","accuracy":"50000","activity_confidence":"1","last_movement":"1972","downthrown_side_dir":"E","vert_sep_rate":"(4.,,)","exposure_quality":"2","notes":"Source of the 1972 Managua Earthquake. Geology indicates mostly normal slip but '72 event was pure left lateral on a very steep plane."},{"average_dip":"(80,70,90)","catalog_id":"CA_249.0","catalog_name":"GEM_Central_Am_Carib","dip_dir":"E","name":"Punta Huete Fault","slip_type":"Sinistral-Normal","reference":"DEM; Brown et al., 1973","epistemic_quality":"2","accuracy":"50000","activity_confidence":"1","downthrown_side_dir":"E","exposure_quality":"2"},{"average_dip":"(90,,)","catalog_id":"CA_250.0","catalog_name":"GEM_Central_Am_Carib","name":"Aguacaliente Fault","slip_type":"Sinistral","reference":"Alonso-Henar 2013","epistemic_quality":"1","accuracy":"60000","activity_confidence":"1","last_movement":"1910","exposure_quality":"1","notes":"paleoseismology suggests recurrence of ~500 years"},{"average_dip":"(65,50,80)","catalog_id":"CA_251.0","catalog_name":"GEM_Central_Am_Carib","dip_dir":"SW","name":"Chiquero Fault","slip_type":"Normal-Dextral","reference":"Montero et al. 2017","epistemic_quality":"1","accuracy":"100000","activity_confidence":"1","downthrown_side_dir":"SW","exposure_quality":"1"},{"average_dip":"(65,50,80)","catalog_id":"CA_252.0","catalog_name":"GEM_Central_Am_Carib","dip_dir":"W","name":"Chiripa Fault","slip_type":"Normal-Dextral","reference":"Montero et al. 2017","epistemic_quality":"1","accuracy":"50000","activity_confidence":"1","downthrown_side_dir":"W","exposure_quality":"2"},{"average_dip":"(60,50,75)","catalog_id":"CA_253.0","catalog_name":"GEM_Central_Am_Carib","dip_dir":"W","name":"Cote-Arenal Fault","slip_type":"Normal-Dextral","reference":"Montero et al. 2017","epistemic_quality":"1","activity_confidence":"1","downthrown_side_dir":"W","exposure_quality":"2"},{"average_dip":"(30,20,50)","catalog_id":"CA_254.0","catalog_name":"GEM_Central_Am_Carib","dip_dir":"S","name":"Upala Fault","slip_type":"Reverse","reference":"Montero et al. 2017","epistemic_quality":"1","accuracy":"50000","activity_confidence":"1","downthrown_side_dir":"N","exposure_quality":"2","notes":"Looks to me like the toe of a big landslide; it's in an otherwise transtensional zone."},{"average_dip":"(90,)","catalog_id":"CA_255.0","catalog_name":"GEM_Central_Am_Carib","name":"Haciendas Fault","slip_type":"Dextral","reference":"Montero et al. 2017","epistemic_quality":"1","accuracy":"50000","activity_confidence":"1","exposure_quality":"1"},{"average_dip":"(30,10,50)","catalog_id":"CA_256.0","catalog_name":"GEM_Central_Am_Carib","dip_dir":"S","slip_type":"Reverse","reference":"Montero et al. 2013","epistemic_quality":"2","accuracy":"50000","activity_confidence":"1","downthrown_side_dir":"N","exposure_quality":"2"},{"average_dip":"(30,20,50)","catalog_id":"CA_257.0","catalog_name":"GEM_Central_Am_Carib","dip_dir":"S","slip_type":"Reverse","reference":"Montero et al. 2013","epistemic_quality":"2","accuracy":"40000","activity_confidence":"1","downthrown_side_dir":"N","exposure_quality":"2"},{"average_dip":"(50,45,70)","catalog_id":"CA_258.0","catalog_name":"GEM_Central_Am_Carib","dip_dir":"SW","name":"Azul Fault","slip_type":"Dextral-Normal","reference":"Montero et al., 2013","epistemic_quality":"1","accuracy":"50000","activity_confidence":"2","downthrown_side_dir":"SW","exposure_quality":"1"},{"average_dip":"(90,,)","catalog_id":"CA_259.0","catalog_name":"GEM_Central_Am_Carib","name":"Kababeta Fault","slip_type":"Dextral","reference":"Montero et al., 2013","epistemic_quality":"2","accuracy":"100000","activity_confidence":"1","exposure_quality":"2"},{"catalog_id":"CA_260.0","catalog_name":"GEM_Central_Am_Carib","name":"Swan Islands Transform","slip_type":"Sinistral_Transform","reference":"Rogers and Mann, 2007","epistemic_quality":"1","accuracy":"1000000","activity_confidence":"1","fs_name":"Swan Islands Transform","strike_slip_rate":"None"},{"catalog_id":"CA_183.0","catalog_name":"GEM_Central_Am_Carib","name":"Swan Islands Transform","slip_type":"Sinistral_Transform","reference":"Rogers and Mann, 2007","epistemic_quality":"1","accuracy":"1000000","activity_confidence":"1","fs_name":"Swan Islands Transform"},{"catalog_id":"CA_262.0","catalog_name":"GEM_Central_Am_Carib","dip_dir":"S","name":"North Caribbean Megathrust (Puerto Rico trench)","net_slip_rate":"(16.5,16,17)","slip_type":"Reverse","reference":"Symithe et al., 2015","activity_confidence":"1","downthrown_side_dir":"N","notes":"Little to no strain accumulation on the fault according to GPS (Symithe et al. 2015). Kinematics probably oblique."},{"average_dip":"(15,10,30)","catalog_id":"CA_nan","catalog_name":"GEM_Central_Am_Carib","dip_dir":"S","name":"North Panama Deformed Belt","slip_type":"Reverse","epistemic_quality":"1","accuracy":"1000000","activity_confidence":"1","downthrown_side_dir":"N","exposure_quality":"2","notes":"Understudied structure.  Poorly mapped on low-resolution bathymetry."},{"average_dip":"(53,40,65)","catalog_id":"MW_31","catalog_name":"SMSSD","dip_dir":"W","name":"Zomba","net_slip_rate":"(0.76,0.077,4.67)","slip_type":"Normal","reference":"Bloomfield (1965); Wedmore et al (2020a)","notes":"Border fault for Zomba Graben. All movement post Cretaceous Lower Chilwa Alkaline Province."},{"average_dip":"(53,40,65)","catalog_id":"MW_26","catalog_name":"SMSSD","dip_dir":"NW","name":"Thyolo","net_slip_rate":"(NA,NA,NA)","slip_type":"Normal","reference":"Habgood, et al (1973); Castaing (1991); Hodge et al (2019); Williams et al (2019); Wedmore et al (2020b)","notes":"Segmented border fault for Lower Shire Basin. Parallel to gneissic foliation. Previously mapped as seperate Thyolo and Muona faults (Hodge et al 2019)."},{"average_dip":"(53,40,65)","catalog_id":"MW_38","catalog_name":"SMSSD","dip_dir":"E","name":"Mtsimukwe","net_slip_rate":"(NA,NA,NA)","slip_type":"Normal","reference":"Bloomfield and Garson (1965); Wedmore et al (2020a)","notes":"Gentle scarp."},{"average_dip":"(53,40,65)","catalog_id":"MW_37","catalog_name":"SMSSD","dip_dir":"E","name":"Mlungusi","net_slip_rate":"(0.08,0.004,0.58)","slip_type":"Normal","reference":"Bloomfield and Garson (1965); Wedmore et al (2020a)","notes":"Steep scarp at base of escarpment. Bounds Shire Horst and Lake Malombe."},{"average_dip":"(53,40,65)","catalog_id":"MW_16","catalog_name":"SMSSD","dip_dir":"SW","name":"Mudi","net_slip_rate":"(0.06,0.004,0.54)","slip_type":"Normal","reference":"Chisenga et al (2019)","notes":"High uncertainity on location, geometry, and activity of fault."},{"average_dip":"(53,40,65)","catalog_id":"MW_43","catalog_name":"SMSSD","dip_dir":"E","name":"Wamkurumadzi","net_slip_rate":"(0.07,0.003,0.55)","slip_type":"Normal","reference":"Bloomfield and Garson (1965)","notes":"Associated with escarpment from 80-300 m in height. Brecciated and silicifed pegmatite at foot of scarp. High uncertainty if active."},{"average_dip":"(53,40,65)","catalog_id":"MW_61","catalog_name":"SMSSD","dip_dir":"W","name":"Cape Maclear","net_slip_rate":"(NA,NA,NA)","slip_type":"Normal","reference":"Dawson and Kirkpatrick (1968)","notes":"Termed the Chingombe Fault by Dawson and Kirkpatrick (1968). Juxtaposes charnockititc gneisses against recent sediments. Eastern tip of fault against syenite intrusion. Parallel to foliation in footwall. Low certainity on whether fault still active."},{"average_dip":"(53,40,65)","catalog_id":"MW_39","catalog_name":"SMSSD","dip_dir":"E","name":"Lisungwe","net_slip_rate":"(0.08,0.005,0.6)","slip_type":"Normal","reference":"Bloomfield and Garson (1965); Wedmore et al (2020a)","notes":"Bounding escarpment 150 m high."},{"average_dip":"(53,40,65)","catalog_id":"MW_45","catalog_name":"SMSSD","dip_dir":"E","name":"Chirobwe-Ncheu","net_slip_rate":"(0.61,0.064,2.92)","slip_type":"Normal","reference":"Dawson and Kirkpatrick (1968); Walshaw (1965)","notes":"Western border fault for the Makanjira Graben."},{"average_dip":"(53,40,65)","catalog_id":"MW_19","catalog_name":"SMSSD","dip_dir":"SW","name":"Elephant Marsh","net_slip_rate":"(NA,NA,NA)","slip_type":"Normal","reference":"Chisenga et al (2019)","notes":"High uncertainity on location, geometry, and activity of fault."},{"average_dip":"(53,40,65)","catalog_id":"MW_2","catalog_name":"SMSSD","dip_dir":"SW","name":"Mwanza","net_slip_rate":"(0.85,0.191,2.24)","slip_type":"Normal","reference":"Castaing (1991); Habgood (1963); Chisenga et al (2019)","notes":"Karoo boundary fault, juxtaposes basement gneisses and alluvium, contains calcite and silicate fault rock. Parallel to gneiss foliation."},{"average_dip":"(53,40,65)","catalog_id":"MW_13","catalog_name":"SMSSD","dip_dir":"NE","name":"Mtumba","net_slip_rate":"(0.06,0.004,0.52)","slip_type":"Normal","reference":"Castaing (1991); Habgood (1963); Chisenga et al (2019)","notes":"This southeastern section mapped from gravity survey."},{"average_dip":"(53,40,65)","catalog_id":"MW_22","catalog_name":"SMSSD","dip_dir":"SW","name":"Ruo","net_slip_rate":"(0.06,0.004,0.53)","slip_type":"Normal","notes":"Minor escarpment, with different sections defined by fault bends. Fault within Mozambique."},{"average_dip":"(53,40,65)","catalog_id":"MW_20","catalog_name":"SMSSD","dip_dir":"SW","name":"Ruo","net_slip_rate":"(0.05,0.003,0.47)","slip_type":"Normal","notes":"Minor escarpment, with different sections defined by fault bends. Fault within Mozambique."},{"average_dip":"(53,40,65)","catalog_id":"MW_21","catalog_name":"SMSSD","dip_dir":"SW","name":"Ruo","net_slip_rate":"(0.07,0.005,0.55)","slip_type":"Normal","notes":"Minor escarpment, with different sections defined by fault bends. Fault within Mozambique."},{"average_dip":"(53,40,65)","catalog_id":"MW_3","catalog_name":"SMSSD","dip_dir":"SW","name":"Mwanza","net_slip_rate":"(0.84,0.185,2.21)","slip_type":"Normal","reference":"Castaing (1991); Habgood (1963); Chisenga et al (2019)","notes":"Eastern extent of this section mapped from aeromag. Karoo boundary fault, juxtaposes basement gneisses and alluvium, contains calcite and silicate fault rock. Parallel to gneiss foliation."},{"average_dip":"(53,40,65)","catalog_id":"MW_4","catalog_name":"SMSSD","dip_dir":"SW","name":"Mwanza","net_slip_rate":"(NA,NA,NA)","slip_type":"Normal","reference":"Castaing (1991); Habgood (1963); Chisenga et al (2019)","notes":"Karoo boundary fault, juxtaposes basement gneisses and alluvium, contains calcite and silicate fault rock. Parallel to gneiss foliation."},{"average_dip":"(53,40,65)","catalog_id":"MW_5","catalog_name":"SMSSD","dip_dir":"SW","name":"Mwanza","net_slip_rate":"(0.9,0.209,2.31)","slip_type":"Normal","reference":"Castaing (1991); Habgood (1963); Chisenga et al (2019)","notes":"Karoo boundary fault, juxtaposes basement gneisses and alluvium, contains calcite and silicate fault rock. Parallel to gneiss foliation."},{"average_dip":"(53,40,65)","catalog_id":"MW_6","catalog_name":"SMSSD","dip_dir":"SW","name":"Mwanza","net_slip_rate":"(NA,NA,NA)","slip_type":"Normal","reference":"Castaing (1991); Habgood (1963); Chisenga et al (2019)","notes":"Karoo boundary fault, juxtaposes basement gneisses and alluvium, contains calcite and silicate fault rock. Parallel to gneiss foliation."},{"average_dip":"(53,40,65)","catalog_id":"MW_7","catalog_name":"SMSSD","dip_dir":"SW","name":"Mwanza","net_slip_rate":"(0.86,0.194,2.25)","slip_type":"Normal","reference":"Castaing (1991); Habgood (1963); Chisenga et al (2019)","notes":"Karoo boundary fault, juxtaposes basement gneisses and alluvium, contains calcite and silicate fault rock. Parallel to gneiss foliation."},{"average_dip":"(53,40,65)","catalog_id":"MW_8","catalog_name":"SMSSD","dip_dir":"SW","name":"Mwanza","net_slip_rate":"(0.39,0.05,1.36)","slip_type":"Normal","reference":"Castaing (1991); Habgood (1963); Chisenga et al (2019)","notes":"Karoo boundary fault, juxtaposes basement gneisses and alluvium, contains calcite and silicate fault rock. Parallel to gneiss foliation."},{"average_dip":"(53,40,65)","catalog_id":"MW_27","catalog_name":"SMSSD","dip_dir":"SW","name":"Thyolo","net_slip_rate":"(0.74,0.107,4.89)","slip_type":"Normal","reference":"Habgood, et al (1973); Castaing (1991); Hodge et al (2019); Williams et al (2019); Wedmore et al (2020b)","notes":"Segmented border fault for Lower Shire Basin. Parallel to gneissic foliation. Previously mapped as seperate Muona fault (Hodge et al 2019)."},{"average_dip":"(53,40,65)","catalog_id":"MW_23","catalog_name":"SMSSD","dip_dir":"SW","name":"Thyolo","net_slip_rate":"(0.78,0.118,4.98)","slip_type":"Normal","reference":"Habgood, et al (1973); Castaing (1991); Hodge et al (2019); Williams et al (2019); Wedmore et al (2020b)","notes":"Segmented border fault for Lower Shire Basin. Parallel to gneissic foliation. Previously mapped as seperate Thyolo and Muona faults (Hodge et al 2019)."},{"average_dip":"(53,40,65)","catalog_id":"MW_25","catalog_name":"SMSSD","dip_dir":"SW","name":"Thyolo","net_slip_rate":"(0.7,0.099,4.77)","slip_type":"Normal","reference":"Habgood, et al (1973); Castaing (1991); Hodge et al (2019); Williams et al (2019); Wedmore et al (2020b)","notes":"Segmented border fault for Lower Shire Basin. Parallel to gneissic foliation. Previously mapped as seperate Thyolo and Muona faults (Hodge et al 2019)."},{"average_dip":"(53,40,65)","catalog_id":"MW_24","catalog_name":"SMSSD","dip_dir":"SW","name":"Thyolo","net_slip_rate":"(0.69,0.095,4.71)","slip_type":"Normal","reference":"Habgood, et al (1973); Castaing (1991); Hodge et al (2019); Williams et al (2019); Wedmore et al (2020b)","notes":"Segmented border fault for Lower Shire Basin. Parallel to gneissic foliation. Previously mapped as seperate Thyolo and Muona faults (Hodge et al 2019)."},{"average_dip":"(53,40,65)","catalog_id":"MW_17","catalog_name":"SMSSD","dip_dir":"NE","name":"Mudi","net_slip_rate":"(NA,NA,NA)","slip_type":"Normal","reference":"Chisenga et al (2019)","notes":"High uncertainity on location, geometry, and activity of fault."},{"average_dip":"(53,40,65)","catalog_id":"MW_18","catalog_name":"SMSSD","dip_dir":"SW","name":"Mudi","net_slip_rate":"(0.07,0.005,0.55)","slip_type":"Normal","reference":"Chisenga et al (2019)","notes":"High uncertainity on location, geometry, and activity of fault."},{"average_dip":"(53,40,65)","catalog_id":"MW_14","catalog_name":"SMSSD","dip_dir":"NE","name":"Mtumba","net_slip_rate":"(NA,NA,NA)","slip_type":"Normal","reference":"Castaing (1991); Habgood (1963); Chisenga et al (2019)","notes":"Mapped from minor escarpment with eastern extent of trace mapped from gravity survey."},{"average_dip":"(53,40,65)","catalog_id":"MW_15","catalog_name":"SMSSD","dip_dir":"NE","name":"Mtumba","net_slip_rate":"(0.06,0.004,0.54)","slip_type":"Normal","reference":"Castaing (1991); Habgood (1963); Chisenga et al (2019)","notes":"Mapped from minor escarpment with southeastern section mapped from gravity survey."},{"average_dip":"(53,40,65)","catalog_id":"MW_42","catalog_name":"SMSSD","dip_dir":"E","name":"Wamkurumadzi","net_slip_rate":"(0.08,0.004,0.59)","slip_type":"Normal","reference":"Bloomfield and Garson (1965)","notes":"Associated with escarpment from 80-300 m in height. Brecciated and silicifed pegmatite at foot of scarp. High uncertainty if active."},{"average_dip":"(53,40,65)","catalog_id":"MW_40","catalog_name":"SMSSD","dip_dir":"E","name":"Lisungwe","net_slip_rate":"(NA,NA,NA)","slip_type":"Normal","reference":"Bloomfield and Garson (1965); Wedmore et al (2020a)","notes":"Bounding escarpment 150 m high. High uncertainity of whether is linkage is 'hard' or 'soft.'"},{"average_dip":"(53,40,65)","catalog_id":"MW_41","catalog_name":"SMSSD","dip_dir":"E","name":"Lisungwe","net_slip_rate":"(0.07,0.004,0.56)","slip_type":"Normal","reference":"Bloomfield and Garson (1965); Wedmore et al (2020a)","notes":"Bounding escarpment 150 m high."},{"average_dip":"(53,40,65)","catalog_id":"MW_35","catalog_name":"SMSSD","dip_dir":"E","name":"Mlungusi","net_slip_rate":"(0.07,0.004,0.55)","slip_type":"Normal","reference":"Bloomfield and Garson (1965); Wedmore et al (2020a)","notes":"Laterally continuous scarp mapped as terrace by Bloomfield and Garson (1965)."},{"average_dip":"(53,40,65)","catalog_id":"MW_36","catalog_name":"SMSSD","dip_dir":"E","name":"Mlungusi","net_slip_rate":"(0.07,0.004,0.56)","slip_type":"Normal","reference":"Bloomfield and Garson (1965); Wedmore et al (2020a)","notes":"Laterally continuous scarp mapped as terrace by Bloomfield and Garson (1965)."},{"average_dip":"(53,40,65)","catalog_id":"MW_32","catalog_name":"SMSSD","dip_dir":"NW","name":"Chingale Step","net_slip_rate":"(0.06,0.003,0.48)","slip_type":"Normal","reference":"Bloomfield (1965); Williams et al (2019); Wedmore et al (2020a)","notes":"Near pure normal slip slickenslides. Labelled Mpimbi fault by Bloomfield (1965)."},{"average_dip":"(53,40,65)","catalog_id":"MW_28","catalog_name":"SMSSD","dip_dir":"W","name":"Zomba","net_slip_rate":"(0.76,0.077,4.67)","slip_type":"Normal","reference":"Bloomfield (1965); Wedmore et al (2020a)","notes":"This section mapped from aeromag data. Border fault for Zomba Graben. All movement post Cretaceous Lower Chilwa Alkaline Province."},{"average_dip":"(53,40,65)","catalog_id":"MW_30","catalog_name":"SMSSD","dip_dir":"W","name":"Zomba","net_slip_rate":"(0.72,0.071,4.52)","slip_type":"Normal","reference":"Bloomfield (1965); Wedmore et al (2020a)","notes":"Border fault for Zomba Graben. All movement post Cretaceous Lower Chilwa Alkaline Province."},{"average_dip":"(53,40,65)","catalog_id":"MW_29","catalog_name":"SMSSD","dip_dir":"W","name":"Zomba","net_slip_rate":"(0.75,0.075,4.62)","slip_type":"Normal","reference":"Bloomfield (1965); Wedmore et al (2020a)","notes":"Border fault for Zomba Graben. All movement post Cretaceous Lower Chilwa Alkaline Province."},{"average_dip":"(53,40,65)","catalog_id":"MW_67","catalog_name":"SMSSD","dip_dir":"W","name":"Makanjira","net_slip_rate":"(0.55,0.05,2.8)","slip_type":"Normal","reference":"Manyozo et al (1972); King and Dawson (1976); Dulanya et al (2017)","notes":"Eastern border fault for the Makanjira Graben. Highly segmented fault system with variable exposure quality."},{"average_dip":"(53,40,65)","catalog_id":"MW_68","catalog_name":"SMSSD","dip_dir":"W","name":"Makanjira","net_slip_rate":"(NA,NA,NA)","slip_type":"Normal","reference":"Manyozo et al (1972); King and Dawson (1976); Dulanya et al (2017)","notes":"Eastern border fault for the Makanjira Graben. Highly segmented fault system with variable exposure quality."},{"average_dip":"(53,40,65)","catalog_id":"MW_69","catalog_name":"SMSSD","dip_dir":"W","name":"Makanjira","net_slip_rate":"(0.62,0.065,2.76)","slip_type":"Normal","reference":"Manyozo et al (1972); King and Dawson (1976); Dulanya et al (2017)","notes":"Eastern border fault for the Makanjira Graben. Highly segmented fault system with variable exposure quality."},{"average_dip":"(53,40,65)","catalog_id":"MW_70","catalog_name":"SMSSD","dip_dir":"W","name":"Makanjira","net_slip_rate":"(NA,NA,NA)","slip_type":"Normal","reference":"Manyozo et al (1972); King and Dawson (1976); Dulanya et al (2017)","notes":"Eastern border fault for the Makanjira Graben. Highly segmented fault system with variable exposure quality."},{"average_dip":"(53,40,65)","catalog_id":"MW_71","catalog_name":"SMSSD","dip_dir":"W","name":"Makanjira","net_slip_rate":"(NA,NA,NA)","slip_type":"Normal","reference":"Manyozo et al (1972); King and Dawson (1976); Dulanya et al (2017)","notes":"Eastern border fault for the Makanjira Graben. Highly segmented fault system with variable exposure quality."},{"average_dip":"(53,40,65)","catalog_id":"MW_72","catalog_name":"SMSSD","dip_dir":"W","name":"Makanjira","net_slip_rate":"(0.62,0.065,2.76)","slip_type":"Normal","reference":"Manyozo et al (1972); King and Dawson (1976); Dulanya et al (2017)","notes":"Eastern border fault for the Makanjira Graben. Highly segmented fault system with variable exposure quality."},{"average_dip":"(53,40,65)","catalog_id":"MW_62","catalog_name":"SMSSD","dip_dir":"E","name":"Malombe","net_slip_rate":"(0.13,0.006,0.81)","slip_type":"Normal","reference":"Manyozo et al (1972); Hodge et al (2019)","notes":"Steep scarp at base of escarpment. Bounds Shire Horst and Lake Malombe."},{"average_dip":"(53,40,65)","catalog_id":"MW_66","catalog_name":"SMSSD","dip_dir":"E","name":"Malombe","net_slip_rate":"(0.08,0.003,0.63)","slip_type":"Normal","reference":"Manyozo et al (1972); Hodge et al (2019)","notes":"Steep scarp at base of escarpment. Bounds Shire Horst and Lake Malombe."},{"average_dip":"(53,40,65)","catalog_id":"MW_63","catalog_name":"SMSSD","dip_dir":"E","name":"Malombe","net_slip_rate":"(0.13,0.006,0.8)","slip_type":"Normal","reference":"Manyozo et al (1972); Hodge et al (2019)","notes":"Steep scarp at base of escarpment. Bounds Shire Horst and Lake Malombe."},{"average_dip":"(53,40,65)","catalog_id":"MW_64","catalog_name":"SMSSD","dip_dir":"E","name":"Malombe","net_slip_rate":"(NA,NA,NA)","slip_type":"Normal","reference":"Manyozo et al (1972); Hodge et al (2019)","notes":"Steep scarp at base of escarpment. Bounds Shire Horst and Lake Malombe."},{"average_dip":"(53,40,65)","catalog_id":"MW_59","catalog_name":"SMSSD","dip_dir":"NE","name":"Bilila-Mtakataka","net_slip_rate":"(0.13,0.006,0.8)","slip_type":"Normal","reference":"Walshaw (1965); Dawson and Kirkpatrick (1968); Jackson and Blenkinsop (1997); Hodge et al (2018, 2019, 2020); Williams et al (2019)","notes":"Laterally continuous steep scarp suggests recent, possibly Late Quaternary, events (Hodge et al 2020)."},{"average_dip":"(53,40,65)","catalog_id":"MW_46","catalog_name":"SMSSD","dip_dir":"E","name":"Chirobwe-Ncheu","net_slip_rate":"(0.61,0.064,2.92)","slip_type":"Normal","reference":"Dawson and Kirkpatrick (1968); Walshaw (1965)","notes":"Scarp along this section. Western border fault for the Makanjira Graben."},{"average_dip":"(53,40,65)","catalog_id":"MW_47","catalog_name":"SMSSD","dip_dir":"E","name":"Chirobwe-Ncheu","net_slip_rate":"(0.61,0.064,2.91)","slip_type":"Normal","reference":"Dawson and Kirkpatrick (1968); Walshaw (1965)","notes":"Western border fault for the Makanjira Graben."},{"average_dip":"(53,40,65)","catalog_id":"MW_48","catalog_name":"SMSSD","dip_dir":"E","name":"Chirobwe-Ncheu","net_slip_rate":"(NA,NA,NA)","slip_type":"Normal","reference":"Dawson and Kirkpatrick (1968); Walshaw (1965)","notes":"Western border fault for the Makanjira Graben."},{"average_dip":"(53,40,65)","catalog_id":"MW_49","catalog_name":"SMSSD","dip_dir":"E","name":"Chirobwe-Ncheu","net_slip_rate":"(0.6,0.065,2.9)","slip_type":"Normal","reference":"Dawson and Kirkpatrick (1968); Walshaw (1965)","notes":"Western border fault for the Makanjira Graben."},{"average_dip":"(53,40,65)","catalog_id":"MW_50","catalog_name":"SMSSD","dip_dir":"E","name":"Chirobwe-Ncheu","net_slip_rate":"(NA,NA,NA)","slip_type":"Normal","reference":"Dawson and Kirkpatrick (1968); Walshaw (1965)","notes":"Western border fault for the Makanjira Graben."},{"average_dip":"(53,40,65)","catalog_id":"MW_54","catalog_name":"SMSSD","dip_dir":"NE","name":"Bilila-Mtakataka","net_slip_rate":"(0.13,0.006,0.81)","slip_type":"Normal","reference":"Walshaw (1965); Dawson and Kirkpatrick (1968); Jackson and Blenkinsop (1997); Hodge et al (2018, 2019, 2020); Williams et al (2019)","notes":"Laterally continuous steep scarp suggests recent, possibly Late Quaternary, events (Hodge et al 2020)."},{"average_dip":"(53,40,65)","catalog_id":"MW_60","catalog_name":"SMSSD","dip_dir":"NE","name":"Bilila-Mtakataka","net_slip_rate":"(0.13,0.006,0.8)","slip_type":"Normal","reference":"Walshaw (1965); Dawson and Kirkpatrick (1968); Jackson and Blenkinsop (1997); Hodge et al (2018, 2019, 2020); Williams et al (2019)","notes":"High uncertainity on activity of this seciton"},{"average_dip":"(53,40,65)","catalog_id":"MW_33","catalog_name":"SMSSD","dip_dir":"NW","name":"Chingale Step","net_slip_rate":"(0.08,0.004,0.57)","slip_type":"Normal","reference":"Bloomfield (1965); Williams et al (2019); Wedmore et al (2020a)","notes":"Near pure normal slip slickenslides. Labelled Mpimbi fault by Bloomfield (1965)."},{"average_dip":"(53,40,65)","catalog_id":"MW_34","catalog_name":"SMSSD","dip_dir":"NW","name":"Chingale Step","net_slip_rate":"(0.07,0.003,0.54)","slip_type":"Normal","reference":"Bloomfield (1965); Williams et al (2019); Wedmore et al (2020a)","notes":"Near pure normal slip slickenslides. Labelled Mpimbi fault by Bloomfield (1965)."},{"average_dip":"(53,40,65)","catalog_id":"MW_73","catalog_name":"SMSSD","dip_dir":"W","name":"Makanjira","net_slip_rate":"(0.6,0.065,2.55)","slip_type":"Normal","reference":"Manyozo et al (1972); King and Dawson (1976); Dulanya et al (2017)","notes":"Eastern border fault for the Makanjira Graben. Highly segmented fault system with variable exposure quality."},{"average_dip":"(53,40,65)","catalog_id":"MW_74","catalog_name":"SMSSD","dip_dir":"W","name":"Makanjira","net_slip_rate":"(0.61,0.059,2.92)","slip_type":"Normal","reference":"Manyozo et al (1972); King and Dawson (1976); Dulanya et al (2017)","notes":"Eastern border fault for the Makanjira Graben. Highly segmented fault system with variable exposure quality."},{"average_dip":"(53,40,65)","catalog_id":"MW_65","catalog_name":"SMSSD","dip_dir":"E","name":"Malombe","net_slip_rate":"(0.13,0.006,0.78)","slip_type":"Normal","reference":"Manyozo et al (1972); Hodge et al (2019)","notes":"Steep scarp at base of escarpment. Bounds Shire Horst and Lake Malombe."},{"average_dip":"(53,40,65)","catalog_id":"MW_51","catalog_name":"SMSSD","dip_dir":"E","name":"Chirobwe-Ncheu","net_slip_rate":"(0.62,0.062,2.91)","slip_type":"Normal","reference":"Dawson and Kirkpatrick (1968); Walshaw (1965)","notes":"High uncertainity in location and extent of this section. Western border fault for the Makanjira Graben."},{"average_dip":"(53,40,65)","catalog_id":"MW_52","catalog_name":"SMSSD","dip_dir":"E","name":"Chirobwe-Ncheu","net_slip_rate":"(0.62,0.053,2.69)","slip_type":"Normal","reference":"Dawson and Kirkpatrick (1968); Walshaw (1965)","notes":"Western border fault for the Makanjira Graben."},{"average_dip":"(53,40,65)","catalog_id":"MW_53","catalog_name":"SMSSD","dip_dir":"E","name":"Chirobwe-Ncheu","net_slip_rate":"(NA,NA,NA)","slip_type":"Normal","reference":"Dawson and Kirkpatrick (1968); Walshaw (1965)","notes":"Scarp along this section. Western border fault for the Makanjira Graben."},{"average_dip":"(53,40,65)","catalog_id":"MW_55","catalog_name":"SMSSD","dip_dir":"NE","name":"Bilila-Mtakataka","net_slip_rate":"(0.12,0.006,0.66)","slip_type":"Normal","reference":"Walshaw (1965); Dawson and Kirkpatrick (1968); Jackson and Blenkinsop (1997); Hodge et al (2018, 2019, 2020); Williams et al (2019)","notes":"Laterally continuous steep scarp suggests recent, possibly Late Quaternary, events (Hodge et al 2020)."},{"average_dip":"(53,40,65)","catalog_id":"MW_56","catalog_name":"SMSSD","dip_dir":"NE","name":"Bilila-Mtakataka","net_slip_rate":"(0.12,0.005,0.79)","slip_type":"Normal","reference":"Walshaw (1965); Dawson and Kirkpatrick (1968); Jackson and Blenkinsop (1997); Hodge et al (2018, 2019, 2020); Williams et al (2019)","notes":"Laterally continuous steep scarp suggests recent, possibly Late Quaternary, events (Hodge et al 2020)."},{"average_dip":"(53,40,65)","catalog_id":"MW_9","catalog_name":"SMSSD","dip_dir":"NE","name":"Panga-1","net_slip_rate":"(NA,NA,NA)","slip_type":"Normal","reference":"Castaing (1991); Habgood (1963); Chisenga et al (2019)","notes":"Part of larger Panga Fault System a Karoo age structure that juxtaposes Karoo sediments and lavas in the footwall against Cretaceous sediments and recent alluvium. Intruded and subsequently deforms dyke, active pre and post Karoo."},{"average_dip":"(53,40,65)","catalog_id":"MW_10","catalog_name":"SMSSD","dip_dir":"NE","name":"Panga-2","net_slip_rate":"(NA,NA,NA)","slip_type":"Normal","reference":"Castaing (1991); Habgood (1963); Chisenga et al (2019)","notes":"Part of larger Panga Fault System, a Karoo age structure that juxtaposes Karoo sediments and lavas in the footwall against Cretaceous sediments and recent alluvium. Intruded and subsequently deforms dyke, active pre and post Karoo."},{"average_dip":"(53,40,65)","catalog_id":"MW_11","catalog_name":"SMSSD","dip_dir":"NE","name":"Panga-3","net_slip_rate":"(NA,NA,NA)","slip_type":"Normal","reference":"Castaing (1991); Habgood (1963); Chisenga et al (2019)","notes":"Part of larger Panga Fault System, a Karoo age structure that juxtaposes Karoo sediments and lavas in the footwall against Cretaceous sediments and recent alluvium. Intruded and subsequently deforms dyke, active pre and post Karoo."},{"average_dip":"(53,40,65)","catalog_id":"MW_12","catalog_name":"SMSSD","dip_dir":"NE","name":"Panga-4","net_slip_rate":"(NA,NA,NA)","slip_type":"Normal","reference":"Castaing (1991); Habgood (1963); Chisenga et al (2019)","notes":"Part of larger Panga Fault System, a Karoo age structure that juxtaposes Karoo sediments and lavas in the footwall against Cretaceous sediments and recent alluvium. Intruded and subsequently deforms dyke, active pre and post Karoo."},{"average_dip":"(53,40,65)","catalog_id":"MW_44","catalog_name":"SMSSD","dip_dir":"E","name":"Tsikulamowa","net_slip_rate":"(NA,NA,NA)","slip_type":"Normal","reference":"Walshaw (1965); Bloomfield and Garson (1965)","notes":"Fault does not follow foliation, relatively prominent scarp 60 m high. No or very thin (<1 m) sediments in hanging wall on geological map, confirmed by fieldwork."},{"average_dip":"(53,40,65)","catalog_id":"MW_1","catalog_name":"SMSSD","dip_dir":"E","name":"Nsanje","net_slip_rate":"(NA,NA,NA)","slip_type":"Normal","reference":"Bloomfield (1957)","notes":"Northern extent of Urema Graben."},{"average_dip":"(53,40,65)","catalog_id":"MW_58","catalog_name":"SMSSD","dip_dir":"NE","name":"Bilila-Mtakataka","net_slip_rate":"(0.13,0.006,0.8)","slip_type":"Normal","reference":"Walshaw (1965); Dawson and Kirkpatrick (1968); Jackson and Blenkinsop (1997); Hodge et al (2018, 2019, 2020); Williams et al (2019)","notes":"Laterally continuous steep scarp suggests recent, possibly Late Quaternary, events (Hodge et al 2020)."},{"average_dip":"(53,40,65)","catalog_id":"MW_57","catalog_name":"SMSSD","dip_dir":"NE","name":"Bilila-Mtakataka","net_slip_rate":"(0.13,0.006,0.81)","slip_type":"Normal","reference":"Walshaw (1965); Dawson and Kirkpatrick (1968); Jackson and Blenkinsop (1997); Hodge et al (2018, 2019, 2020); Williams et al (2019)","notes":"Laterally continuous steep scarp suggests recent, possibly Late Quaternary, events (Hodge et al 2020)."}]