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DOI10.6038/cjg20150116
Rupture process of 12 February 2014, Yutian M(w)6. 9 earthquake and stress change on nearby faults
Zhou Yun; Wang Wei-Min; Xiong Lin; He Jian-Kun
通讯作者Zhou, Y (通讯作者)
发表日期2015
ISSN0001-5733
起始页码184
结束页码193
卷号58期号:1
英文摘要On February 12 2014, an M(s)7. 3 earthquake hit Yutian, Xinjiang, the epicenter is at the intersection of Karakax fault and Gonggacuo fault. Earthquake triggering theory indicates that Coulomb stress on nearby faults will change because of crustal coseismic slip after earthquake, and it will affect earthquake potential risk. In this paper, we estimate focal mechanism and rupture process with far field seismic wave data, and calculate coseismic stress change on nearby faults around epicenter. The purpose is to discuss Coulomb stress change and seismic potential hazard on these faults caused by Yutian earthquake. After the earthquake, we download seismic far field wave data of which epicenter is between 30 degrees to 90 degrees from IRIS. We select 27 high SNR (signal to noise ratio) seismic record to make theoretical seismogram. We use generalized ray theory to get synthetic seismic wave map, and sub fault parameter inverse process is based on simulated annealing algorithms. In the way of changing fault parameter to fit actual and synthetic wave form, optimum solution of every sub fault is found. Based on fault rupture inversion model and infinite elastic half space theory, we calculate Coulomb stress change on nearby faults caused by the earthquake. The inversion results show that source depth of earthquake is 10 km, dip angle is 71. 9 degrees, largest coseismic displacement is 210 cm. Seismic moment is 2.91 X 10(19)N . m, the main seismic energy is released in former 10 second. Aftershocks are mainly distributed in three regions, north Pulu fault, east Karakax fault and centre Gonggacuo fault. Stress increased significantly on western segment of Altyn fault, central part of Pulu fault, eastern segment of Karakax fault and central segment of Gonggacuo fault. Among them the largest stress change is 0. 05 MPa on Karakax fault and 0. 04 MPa on Gonggacuo fault. Former research shows that, Coulomb stress change caused by earthquake larger than 0. 01 MPa will dramatically increase seismic risk on faults. In our research, stress change on Pulu fault, Gonggacuo fault and Karakax fault exceed triggering threshold, so all these three faults have seismic risk. In the near future seismic potential hazard on these faults should be closely monitored. In the past 6 years, 3 moderately strong earthquakes happen in the study area, epicenters migrate from Gonggacuo fault to Altyn fault, from southwest to northeast. Though stress change on Altyn fault is much lower, in consideration of 9 mm . a(-1) slip rate, seismic risk on Altyn fault should cause enough attention.
关键词SAN-ANDREAS FAULTALTYN-TAGH FAULTWENCHUAN EARTHQUAKESLIPMODELCYCLEDEFORMATIONCALIFORNIAEVOLUTIONFAILURE
英文关键词Yutian earthquake in 2014; Coseismic rupture; Coulomb stress; Seismic hazard
语种英语
WOS研究方向Geochemistry & Geophysics
WOS类目Geochemistry & Geophysics
WOS记录号WOS:000349136200016
来源期刊CHINESE JOURNAL OF GEOPHYSICS-CHINESE EDITION
来源机构中国科学院青藏高原研究所
文献类型期刊论文
条目标识符http://gcip.llas.ac.cn/handle/2XKMVOVA/258419
推荐引用方式
GB/T 7714
Zhou Yun,Wang Wei-Min,Xiong Lin,et al. Rupture process of 12 February 2014, Yutian M(w)6. 9 earthquake and stress change on nearby faults[J]. 中国科学院青藏高原研究所,2015,58(1).
APA Zhou Yun,Wang Wei-Min,Xiong Lin,&He Jian-Kun.(2015).Rupture process of 12 February 2014, Yutian M(w)6. 9 earthquake and stress change on nearby faults.CHINESE JOURNAL OF GEOPHYSICS-CHINESE EDITION,58(1).
MLA Zhou Yun,et al."Rupture process of 12 February 2014, Yutian M(w)6. 9 earthquake and stress change on nearby faults".CHINESE JOURNAL OF GEOPHYSICS-CHINESE EDITION 58.1(2015).
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