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Aftershock analysis of the 2015 Gorkha-Dolakha (Central Nepal) earthquake doublet

机译:2015年尼泊尔中部(Gorkha-Dolakha)地震双重地震的余震分析

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摘要

On 25 April 2015, a large earthquake with moment>-magnitude (Mw) 7.8 occurred at Gorkha (latitude 28.23° N and longitude 84.73° E) in Central Nepal. Just 17 days later, another large earthquake of Mw 7.3 occurred at Dolakha (latitude 27.80° N and longitude 86.06° E), about 140 km away from the previous epicenter. In this study, we deal with the aftershocks of these two earthquakes that occurred in the region (27°–28.5°N, 84°–87°E) spanning the period from 25 April 2015 to 28 May 2016 to find the spatiotemporal distribution patterns, the size distribution (b-value), and the aftershock decay rate (p-value) of this sequence. Aftershock epicenters of the 2015 Gorkha-Dolakha earthquake doublet are distributed over an area approximately 170 km in length and 70 km in width and largely confined in a depth range from 5 to 25 km. The spatial distribution of epicenters and known geological structures in this study reveals that aftershocks are limited on the east by the surface trace of the Everest lineament and on the south side by the surface trace of the segment of the Main Boundary Thrust (MBT). The estimated b-and p-values of this seismic sequence are 0.93 ± 0.03 and 0.79 ± 0.24, respectively. This b-value is higher than the b-value estimated by the previous studies, while the p-value corresponds in general with the p-value obtained by recent study in the region.
机译:2015年4月25日,尼泊尔中部戈尔卡(北纬28.23°,东经84.73°)发生了矩>-震级(Mw)7.8的大地震。仅仅17天后,又一次地震发生在Dolakha(北纬27.80°,东经86.06°E),距先前震中约140公里,发生7.3兆瓦地震。在这项研究中,我们处理了2015年4月25日至2016年5月28日期间在该地区(27°–28.5°N,84°–87°E)发生的两次地震的余震,以发现时空分布模式,大小分布(b值)和此序列的余震衰减率(p值)。 2015年Gorkha-Dolakha地震双重震的余震震中分布在长约170 km,宽约70 km的区域内,且深度限于5至25 km。这项研究的震中和已知地质结构的空间分布表明,余震在东部受到珠穆朗玛峰地表的表面痕迹的限制,而在南侧受到主边界推力(MBT)段的表面痕迹的限制。该地震序列的估计b值和p值分别为0.93±0.03和0.79±0.24。该b值高于先前研究估计的b值,而p值通常与该地区最近研究获得的p值相对应。

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