Seismogenic Structure and Tectonic Mechanism of the 2021 Mw 5.0 Yancheng Earthquake in the South Yellow Sea Basin, East Asia

Author:

Hu Panpan12ORCID,Yang Xiaodong345,Yang Fengli12,Zhang Jinchang345,Zhou Zhiyuan6,Dong Ruowen12

Affiliation:

1. 1State Key Laboratory of Marine Geology, Tongji University, Shanghai, China

2. 2School of Ocean and Earth Science, Tongji University, Shanghai, China

3. 3CAS Key Laboratory of Ocean and Marginal Sea Geology, South China Sea Institute of Oceanology, Innovation Academy of South China Sea Ecology and Environmental Engineering, Chinese Academy of Sciences, Guangzhou, China

4. 4Southern Marine Science and Engineering Guangdong Laboratory (Guangzhou), Guangzhou, China

5. 5China-Pakistan Joint Research Center on Earth Science, CAS-HEC, Islamabad, Pakistan

6. 6Guangzhou Urban Planning Survey and Design Institute, Guangzhou, China

Abstract

AbstractOn 17 November 2021, a moment magnitude (Mw) 5.0 earthquake occurred off the Yancheng city in the South Yellow Sea. This earthquake has caused ground motions and been felt by people in a few megacities in east China, for example, Shanghai, Nanjing. However, due to limited seismic data, the focal fault and mechanism of this earthquake remain unknown. Here, we combine the seismic profiles, seismicity, focal mechanism, well data with regional tectonics to investigate the seismotectonics of this event and the possible role of fluid migration in triggering the earthquake. Our new results suggest that two sets of preexisting strike-slip faults were developed near the epicenter of the Yancheng earthquake, including the north–northeast-trending fault F1, the North Wunansha fault, and the northwest-trending fault F5. These preexisting faults have been reactivated entirely or partly with dextral and sinistral motions during the Miocene to Quaternary. Fault F1 runs through the epicenter of the Yancheng earthquake and is therefore interpreted to be the seismogenic fault. Various igneous complexes and associated hydrothermal vent complexes have been identified in the vicinity of the reactivated fault F1 and other strike-slip faults. Combined with the published igneous rock ages from nearby region, the igneous and hydrothermal activities were suggested to be continue until the Miocene and Quaternary, which are coincident with the reactivation of the preexisting strike-slip faults. The reactivation of the preexisting fault, and igneous and associated hydrothermal activities were suggested to be caused by the subduction of Pacific and Philippine Sea plates and collision of India and Eurasia plate. The hydrothermal fluids may have migrated through the preexisting fault F1 and other strike-slip faults, which enhanced the reactivation of these faults and in turn promoted the fault slip, eventually triggering the Yancheng earthquake and other historical events in the study area.

Publisher

Seismological Society of America (SSA)

Subject

Geophysics

Reference138 articles.

1. When and where did India and Asia collide?;Aitchison;J. Geophys. Res.,2007

2. Cenozoic magmatism in Mongolia and the origin of central and East Asian basalts;Barry;Mantle Dynam. Plate Interact. East Asia,1998

3. Fluid-induced aseismic fault slip outpaces pore-fluid migration;Bhattacharya;Science,2019

4. New constraints on mechanisms of remotely triggered seismicity at Long Valley Caldera;Brodsky;J. Geophys. Res.,2005

5. Cenozoic basaltic rocks in north Jiangsu basin and surrounding area and their bearing on tectonic environment;Chen;J. Fujian Norm. Univ.,1992

Cited by 3 articles. 订阅此论文施引文献 订阅此论文施引文献,注册后可以免费订阅5篇论文的施引文献,订阅后可以查看论文全部施引文献

同舟云学术

1.学者识别学者识别

2.学术分析学术分析

3.人才评估人才评估

"同舟云学术"是以全球学者为主线,采集、加工和组织学术论文而形成的新型学术文献查询和分析系统,可以对全球学者进行文献检索和人才价值评估。用户可以通过关注某些学科领域的顶尖人物而持续追踪该领域的学科进展和研究前沿。经过近期的数据扩容,当前同舟云学术共收录了国内外主流学术期刊6万余种,收集的期刊论文及会议论文总量共计约1.5亿篇,并以每天添加12000余篇中外论文的速度递增。我们也可以为用户提供个性化、定制化的学者数据。欢迎来电咨询!咨询电话:010-8811{复制后删除}0370

www.globalauthorid.com

TOP

Copyright © 2019-2024 北京同舟云网络信息技术有限公司
京公网安备11010802033243号  京ICP备18003416号-3