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- W4311702722 abstract "SUMMARY On 2013 September 24, an earthquake of magnitude Mw 7.7 occurred on the Hoshab Fault in southern Pakistan, south of the 650-km-long Chaman Fault, within the eastern Makran accretionary wedge. This earthquake was caused predominantly by strike-slip faulting. To quantify the post-seismic deformation following this large earthquake, we used ascending and descending Sentinel-1 data over the period 2014 November–2017 December. The deformation time-series over these 3 years shows that the post-seismic deformation was not linear over the time. To determine the mechanisms that may have driven post-seismic deformation, such as after-slip or a combination of after-slip and viscous relaxation, we explored some models, including after-slip only, and a combination of after-slip and viscous relaxation, to identify the best fit between the observed and simulated deformation time-series. Our results indicate that after-slip was the main mechanism controlling the post-seismic deformation. The introduction of a basal flat fault in the modelling improves the fit between the model results and the time-series obtained from the satellite images This basal fault is located at a depth of 18 km, has a northward dip of 7° and corresponds to the basal décollement level of the Makran accretionary prism." @default.
- W4311702722 created "2022-12-28" @default.
- W4311702722 creator A5050325503 @default.
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- W4311702722 date "2022-12-06" @default.
- W4311702722 modified "2023-09-25" @default.
- W4311702722 title "Quantification and modelling of post-seismic deformation following the 2013 September 24 <i>M</i>w 7.7 earthquake in the Makran region, Pakistan" @default.
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- W4311702722 doi "https://doi.org/10.1093/gji/ggac484" @default.
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