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Rupture process of the 2015 Pishan earthquake from joint inversion of InSAR, teleseismic data and GPS

文献类型：期刊论文

作者Wang, Xun1,2; Wang, Weimin1; Zhao, Junmeng1; Yao, Zhenxing3
刊名SCIENCE CHINA-EARTH SCIENCES
出版日期2018-10-01
卷号61期号:10页码:1467-1481
关键词Pishan earthquake Source process Joint inversion Post-earthquake deformation
ISSN号1674-7313
DOI10.1007/s11430-017-9230-8
英文摘要An earthquake of M(w)6.4 occurred in Pishan County in Xinjiang Province, northwestern Tibetan Plateau, on July 3, 2015. The epicenter was located on an active blind thrust system located at the northern margin of the Western Kunlun Mountain Orogenic Belt southwest of the Tarim Basin. We constructed a shovel-shaped fault model based on the layered-crust model with reference to the seismic reflection profile, and obtained the rupture process of the earthquake from the joint inversion of Interferometric Synthetic Aperture Radar (InSAR) measurements, far-field waveform data, and Global Positioning System (GPS) data. The results show that the seismic fault dips southward with a strike of 109 degrees, and the rupture direction was essentially northward. The fault plane rupture distribution is concentrated, with a maximum recorded slip of 73 cm. The main features of the fault are as follows: low inclination angle (25 degrees-10 degrees), thrust slip at a depth of 9-13 km, rupture propagation time of about 12 s, no significant slip in soft or hard sedimentary layers at 0-4 km depth and propagation from the initial rupture point to the surrounding area with no obvious directionality. The InSAR time-series analysis method is used to determine the deformation rate in the source region within 2 years after the earthquake, and the maximum value is similar to 17 mm yr(-1) in the radar line-of-sight direction. Obvious post-earthquake deformation is evident in the hanging wall, with a similar trend to the coseismic displacement field. These results suggest that the Pishan earthquake has not completely released the accumulated energy of the region, given that the multilayer fold structure above the blind fault is still in a process of slow uplift since the earthquake. Post-earthquake adjustment models and aftershock risk analysis require further study using more independent data.
WOS关键词W 6.4 PISHAN ; NORTHWEST TIBETAN PLATEAU ; WEST KUNLUN RANGE ; RADAR INTERFEROMETRY ; GROUND DEFORMATION ; TARIM BASIN ; SENTINEL-1A ; CHINA ; FAULT ; UPLIFT
资助项目National Natural Science Foundation of China[41474036] ; National Natural Science Foundation of China[41174037] ; 13th Five-year Informatization Plan of Chinese Academy of Sciences[XXH13505-06]
WOS研究方向Geology
语种英语
WOS记录号WOS:000446517200010
出版者SCIENCE PRESS
资助机构National Natural Science Foundation of China ; National Natural Science Foundation of China ; 13th Five-year Informatization Plan of Chinese Academy of Sciences ; 13th Five-year Informatization Plan of Chinese Academy of Sciences ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; 13th Five-year Informatization Plan of Chinese Academy of Sciences ; 13th Five-year Informatization Plan of Chinese Academy of Sciences ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; 13th Five-year Informatization Plan of Chinese Academy of Sciences ; 13th Five-year Informatization Plan of Chinese Academy of Sciences ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; 13th Five-year Informatization Plan of Chinese Academy of Sciences ; 13th Five-year Informatization Plan of Chinese Academy of Sciences
源URL[http://ir.iggcas.ac.cn/handle/132A11/89197]  
专题地质与地球物理研究所_中国科学院地球与行星物理重点实验室
通讯作者Wang, Weimin
作者单位1.Chinese Acad Sci, Inst Tibetan Plateau Res, Key Lab Continental Collis & Plateau Uplift, Beijing 100101, Peoples R China
2.Univ Chinese Acad Sci, Coll Earth & Planetary Sci, Beijing 100049, Peoples R China
3.Chinese Acad Sci, Inst Geol & Geophys, Beijing 100029, Peoples R China
推荐引用方式
GB/T 7714		 Wang, Xun,Wang, Weimin,Zhao, Junmeng,et al. Rupture process of the 2015 Pishan earthquake from joint inversion of InSAR, teleseismic data and GPS[J]. SCIENCE CHINA-EARTH SCIENCES,2018,61(10):1467-1481.
APA Wang, Xun,Wang, Weimin,Zhao, Junmeng,&Yao, Zhenxing.(2018).Rupture process of the 2015 Pishan earthquake from joint inversion of InSAR, teleseismic data and GPS.SCIENCE CHINA-EARTH SCIENCES,61(10),1467-1481.
MLA Wang, Xun,et al."Rupture process of the 2015 Pishan earthquake from joint inversion of InSAR, teleseismic data and GPS".SCIENCE CHINA-EARTH SCIENCES 61.10(2018):1467-1481.

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来源：地质与地球物理研究所

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