首页> 外文期刊>Journal of Asian earth sciences >Rupture model of Mw 7.8 2015 Gorkha, Nepal earthquake: Constraints from GPS measurements of coseismic offsets
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Rupture model of Mw 7.8 2015 Gorkha, Nepal earthquake: Constraints from GPS measurements of coseismic offsets

机译:2015年尼泊尔7.8级莫尔瓦地震的破裂模型:来自GPS的同震偏移量测量的约束

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We estimate coseismic offsets at 20 sites in India due to the 25 April 2015 Gorkha, Nepal (Mw 7.8) earthquake. Only four sites in the Indian region, immediately to the south of the rupture, showed discernible coseismic horizontal offsets ranging between 3 and 7 mm toward north. We invert these offsets along with 13 other offsets at GPS sites in Nepal and 33 offsets at sites in China, for the estimation of slip distribution on the causative rupture. We assume that rupture occurred on the Main Himalayan Thrust (MHT). In our estimated slip model, high slip reaching 5 m occurred east of the mainshock epicenter, and the slip on rupture terminated close to the Main Boundary Thrust (MBT). Thus the rupture for this earthquake remained blind, increasing the potential for future earthquake in the shallow, updip unruptured part of the MHT. (C) 2016 Elsevier Ltd. All rights reserved.
机译:我们估计,由于2015年4月25日尼泊尔戈尔卡(Mw 7.8)地震,印度20个地点的同震偏移。在印度区域中,紧接在断裂以南的只有四个位置显示出可识别的同震水平偏移,其向北范围为3至7毫米。我们将这些偏移量与尼泊尔GPS站点的其他13个偏移量以及中国站点的33个偏移量一起进行求反,以估算引起破裂的滑动分布。我们假设破裂发生在喜马拉雅山主推力(MHT)上。在我们估计的滑动模型中,在主震震中以东发生了达到5 m的高滑动,并且破裂的滑动在主边界推力(MBT)附近终止。因此,这次地震的破裂仍然是盲目的,增加了MHT浅层,上倾未破裂部分未来发生地震的可能性。 (C)2016 Elsevier Ltd.保留所有权利。

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