2018年印度尼西亚龙目岛地震序列受GPS数据约束的早期震后变形

IF 2.1 3区 地球科学 Q2 GEOCHEMISTRY & GEOPHYSICS
Risya Fauziyyah , Endra Gunawan , Sri Widiyantoro , Irwan Meilano , Syamsuddin
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引用次数: 2

摘要

印度尼西亚龙目岛的全球定位系统(GPS)站显示,2018年龙目岛地震序列发生在2018年7月28日(6.4级)、2018年8月5日(6.9级)、,以及2018年8月19日(Mw 6.3和Mw 6.9)。本研究调查了2018年8月份19日主震后一个月内的后滑和粘弹性松弛的贡献。本研究利用了2018年8月20日至2018年9月19日的连续GPS数据。分析表明,后滑分布在断层的较浅部分,与主震的同震深滑互补。估计了粘弹性弛豫,涉及粘度为9.0×1017 Pa s的引力麦克斯韦粘弹性响应。这项研究还发现,该地区的弹性上地壳深度为50公里。主震后一个月的观测表明,后滑是大部分正在进行的震后变形的原因。尽管粘弹性松弛在一个月的时间里只起到了不显著的作用,但本研究表明,粘弹性松弛预计会随着时间的推移而增加。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Early postseismic deformation of the 2018 Lombok, Indonesia, earthquake sequence constrained by GPS data

Global Positioning System (GPS) stations in Lombok, Indonesia showed postseismic displacement following the 2018 Lombok earthquake sequence which occurred on 28 July 2018 (Mw 6.4), 5 August 2018 (Mw 6.9), 9 August 2018 (Mw 5.9), and the 19 August 2018 (Mw 6.3 and Mw 6.9). This research has investigated the contribution of afterslip and viscoelastic relaxation during the one-month period after the mainshock on 19 August 2018. This study utilizes continuous GPS data available from 20 August 2018–19 September 2018. The analysis reveals that the afterslip was distributed at the shallower portion of the fault, complementary to the deeper coseismic slip of the mainshock. Viscoelastic relaxation, involving a gravitational Maxwell viscoelastic response with viscosity of 9.0 × 1017 Pa s, was estimated. This research also found that the depth of elastic upper crust in this region is 50 km. Observations made during the one-month period after the mainshock revealed that afterslip was responsible for most of the ongoing postseismic deformation. Although the viscoelastic relaxation contributed only insignificantly during the one-month period, this research shows that viscoelastic relaxation is expected to increase with time.

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来源期刊
Journal of Geodynamics
Journal of Geodynamics 地学-地球化学与地球物理
CiteScore
4.60
自引率
0.00%
发文量
21
审稿时长
6-12 weeks
期刊介绍: The Journal of Geodynamics is an international and interdisciplinary forum for the publication of results and discussions of solid earth research in geodetic, geophysical, geological and geochemical geodynamics, with special emphasis on the large scale processes involved.
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