Main shock source parameters obtained in this study and from Barnhart et al. (2014).
| Strike . | Dip . | Rake . | Len. . | Width . | Dep.* . | Long. . | Lat. . | Vel. . | Orig. time** . | X . | Y . | Mw . | Ref. . |
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| (°) . | (°) . | (°) . | (km) . | (km) . | (km) . | (m) . | (m) . | (km s−1) . | (s) . | . | . | . | . |
| 238 | 56 | −102 | - | - | 50.8 | 62.21 | 27.89 | - | - | 7.7 | CMT | ||
| 233 | 59 | −109 | - | - | 80 | 61.99 | 28.03 | - | - | 7.7 | USGS | ||
| 243 | 58 | −95 | - | - | 71.2 | 62.12 | 27.99 | - | - | 7.72 | GFZ | ||
| 232 | 61 | −125 | 250 | 143 | ∼75 | 62.15 | 27.83 | 2.5–2.75 | - | 7.69 | Barnhart et al. (2014) | ||
| 237 ± 5 | 63 ± 2 | −101 ± 6 | - | - | 79 ± 4 | 61.32 | 27.87 | - | - | - | - | 7.71 ± .01 | Teleseismic*** |
| 243 ± 1 | 48 ± 1 | −127 ± 11 | 102 ± 1 | 18 ± 4 | 57 ± 3 | 61.1 | 27.45 | - | - | - | - | 7.71 ± .03 | InSAR *** |
| 240 ± 6 | 60 ± 2 | −106 ± 19 | 116 ± 16 | 16 ± 4 | 54 ± 3 | 61.4 | 27.8 | - | - | - | - | 7.7 ± .06 | InSAR + GNSS*** |
| 234 ± 3 | 64 ± 2 | −111 ± 7 | 97 ± 17 | 17 ± 2 | 56 ± 2 | 61.94 ± 2 | 27.95 ± 2 | 4.5 ± 1 | -1.8 ± 1 | 0.05 ± 24 | 0.95 ± 59 | 7.6 ± .04 | InSAR + Teleseismic + GNSS *** |
| Strike . | Dip . | Rake . | Len. . | Width . | Dep.* . | Long. . | Lat. . | Vel. . | Orig. time** . | X . | Y . | Mw . | Ref. . |
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| (°) . | (°) . | (°) . | (km) . | (km) . | (km) . | (m) . | (m) . | (km s−1) . | (s) . | . | . | . | . |
| 238 | 56 | −102 | - | - | 50.8 | 62.21 | 27.89 | - | - | 7.7 | CMT | ||
| 233 | 59 | −109 | - | - | 80 | 61.99 | 28.03 | - | - | 7.7 | USGS | ||
| 243 | 58 | −95 | - | - | 71.2 | 62.12 | 27.99 | - | - | 7.72 | GFZ | ||
| 232 | 61 | −125 | 250 | 143 | ∼75 | 62.15 | 27.83 | 2.5–2.75 | - | 7.69 | Barnhart et al. (2014) | ||
| 237 ± 5 | 63 ± 2 | −101 ± 6 | - | - | 79 ± 4 | 61.32 | 27.87 | - | - | - | - | 7.71 ± .01 | Teleseismic*** |
| 243 ± 1 | 48 ± 1 | −127 ± 11 | 102 ± 1 | 18 ± 4 | 57 ± 3 | 61.1 | 27.45 | - | - | - | - | 7.71 ± .03 | InSAR *** |
| 240 ± 6 | 60 ± 2 | −106 ± 19 | 116 ± 16 | 16 ± 4 | 54 ± 3 | 61.4 | 27.8 | - | - | - | - | 7.7 ± .06 | InSAR + GNSS*** |
| 234 ± 3 | 64 ± 2 | −111 ± 7 | 97 ± 17 | 17 ± 2 | 56 ± 2 | 61.94 ± 2 | 27.95 ± 2 | 4.5 ± 1 | -1.8 ± 1 | 0.05 ± 24 | 0.95 ± 59 | 7.6 ± .04 | InSAR + Teleseismic + GNSS *** |
* Depth is calculated between the source upper edge and the ground surface (positive downward), referred to in the main text as top depth.
** The origin time is relative to the GCMT earthquake origin time
*** This study.
(X, Y) is the relative position of the nucleation point on the fault to the centre location.
Main shock source parameters obtained in this study and from Barnhart et al. (2014).
| Strike . | Dip . | Rake . | Len. . | Width . | Dep.* . | Long. . | Lat. . | Vel. . | Orig. time** . | X . | Y . | Mw . | Ref. . |
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| (°) . | (°) . | (°) . | (km) . | (km) . | (km) . | (m) . | (m) . | (km s−1) . | (s) . | . | . | . | . |
| 238 | 56 | −102 | - | - | 50.8 | 62.21 | 27.89 | - | - | 7.7 | CMT | ||
| 233 | 59 | −109 | - | - | 80 | 61.99 | 28.03 | - | - | 7.7 | USGS | ||
| 243 | 58 | −95 | - | - | 71.2 | 62.12 | 27.99 | - | - | 7.72 | GFZ | ||
| 232 | 61 | −125 | 250 | 143 | ∼75 | 62.15 | 27.83 | 2.5–2.75 | - | 7.69 | Barnhart et al. (2014) | ||
| 237 ± 5 | 63 ± 2 | −101 ± 6 | - | - | 79 ± 4 | 61.32 | 27.87 | - | - | - | - | 7.71 ± .01 | Teleseismic*** |
| 243 ± 1 | 48 ± 1 | −127 ± 11 | 102 ± 1 | 18 ± 4 | 57 ± 3 | 61.1 | 27.45 | - | - | - | - | 7.71 ± .03 | InSAR *** |
| 240 ± 6 | 60 ± 2 | −106 ± 19 | 116 ± 16 | 16 ± 4 | 54 ± 3 | 61.4 | 27.8 | - | - | - | - | 7.7 ± .06 | InSAR + GNSS*** |
| 234 ± 3 | 64 ± 2 | −111 ± 7 | 97 ± 17 | 17 ± 2 | 56 ± 2 | 61.94 ± 2 | 27.95 ± 2 | 4.5 ± 1 | -1.8 ± 1 | 0.05 ± 24 | 0.95 ± 59 | 7.6 ± .04 | InSAR + Teleseismic + GNSS *** |
| Strike . | Dip . | Rake . | Len. . | Width . | Dep.* . | Long. . | Lat. . | Vel. . | Orig. time** . | X . | Y . | Mw . | Ref. . |
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| (°) . | (°) . | (°) . | (km) . | (km) . | (km) . | (m) . | (m) . | (km s−1) . | (s) . | . | . | . | . |
| 238 | 56 | −102 | - | - | 50.8 | 62.21 | 27.89 | - | - | 7.7 | CMT | ||
| 233 | 59 | −109 | - | - | 80 | 61.99 | 28.03 | - | - | 7.7 | USGS | ||
| 243 | 58 | −95 | - | - | 71.2 | 62.12 | 27.99 | - | - | 7.72 | GFZ | ||
| 232 | 61 | −125 | 250 | 143 | ∼75 | 62.15 | 27.83 | 2.5–2.75 | - | 7.69 | Barnhart et al. (2014) | ||
| 237 ± 5 | 63 ± 2 | −101 ± 6 | - | - | 79 ± 4 | 61.32 | 27.87 | - | - | - | - | 7.71 ± .01 | Teleseismic*** |
| 243 ± 1 | 48 ± 1 | −127 ± 11 | 102 ± 1 | 18 ± 4 | 57 ± 3 | 61.1 | 27.45 | - | - | - | - | 7.71 ± .03 | InSAR *** |
| 240 ± 6 | 60 ± 2 | −106 ± 19 | 116 ± 16 | 16 ± 4 | 54 ± 3 | 61.4 | 27.8 | - | - | - | - | 7.7 ± .06 | InSAR + GNSS*** |
| 234 ± 3 | 64 ± 2 | −111 ± 7 | 97 ± 17 | 17 ± 2 | 56 ± 2 | 61.94 ± 2 | 27.95 ± 2 | 4.5 ± 1 | -1.8 ± 1 | 0.05 ± 24 | 0.95 ± 59 | 7.6 ± .04 | InSAR + Teleseismic + GNSS *** |
* Depth is calculated between the source upper edge and the ground surface (positive downward), referred to in the main text as top depth.
** The origin time is relative to the GCMT earthquake origin time
*** This study.
(X, Y) is the relative position of the nucleation point on the fault to the centre location.
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