中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
Progress in the studies of the seismic gap between the 2008 Wenchuan and 2013 Lushan earthquakes

文献类型:期刊论文

作者Liang ChunTao1,2; Huang YanLing2; Wang ChaoLiang2; Liu ZhiQiang2; Yang YiHai3; Wu Jin4; He FuJun2
刊名CHINESE JOURNAL OF GEOPHYSICS-CHINESE EDITION
出版日期2018-05-01
卷号61期号:5页码:1996-2010
关键词Seismic gap Receiver function Stress inversion Micro-seismicity
ISSN号0001-5733
DOI10.6038/cjg2018M0254
文献子类Article
英文摘要The purpose of this work is to investigate the deep structure beneath the seismic gap between the 2008 Wenchuan and 2013 Lushan earthquakes, discuss the geodynamic process of the movement of materials, and to assess the seismic potential in this region. We have conducted two phases of seismic observations with more than 100 temporary instruments deployed in the last three years. The preliminary results indicate that (1) the seismic gap serves as a transition zone separating two distinct stress regimes, and the fault-parallel stress difference is observed between the two sides of the gap. (2) The receiver function analysis shows that a long belt of Moho uplift extends from the gap to the Longriba fault, roughly aligning with the Barkam fault. The Poisson's ratio is relatively high along this belt. A partial melting at the lower crust along this belt may explain these observations. (3) Beneath the seismic gap, the velocity in the upper crust is relatively low and a thickened lower crust may indicate the existence of partial melting in the lower crust. These two observations may explain the absence of seismicity in the seismic gap. (4) Micro-seismicity was studied using a matched filter method. Given the complete magnitude of earthquakes being lowered from 1.4 to 0.2, the seismic gap is still void of events compared to the two sides of the gap; seismic locations are also obtained by traveltimes recorded by the densest array in the region deployed recently. The seismicity is still void of events, but a linear strip of seismicity was observed to the east of the seismic gap and it aligns roughly with the Dayi fault and/or other blind faults in the region. These faults could be the structure to yield big events in the future. (5) Based on the above observations, we propose a new model to account for the geodynamics of the seismic gap; the fault-parallel stress difference across the gap may imply that the gap is the point where the crust of the eastern Tibetan plateau is being torn apart, resulting in the upwelling of hot mantle materials to produce partial melting in the lower crust. This partial melting may heat up the upper crust beneath the gap and turn the faults in this segment into aseismic. The tearing apart fracture of the crust may extend all the way to the Barkam fault, but it less developed further away from the seismic gap in the Longmenshan fault system.
WOS关键词FOCAL MECHANISM SOLUTIONS ; LOWER CRUSTAL FLOW ; TIBETAN PLATEAU ; LONGMEN SHAN ; TECTONIC DEFORMATION ; EASTERN MARGIN ; STRESS-FIELD ; CHINA ; SEQUENCE ; NORTH
WOS研究方向Geochemistry & Geophysics
语种英语
WOS记录号WOS:000432644000027
出版者SCIENCE PRESS
源URL[http://ir.iggcas.ac.cn/handle/132A11/88243]  
专题中国科学院地质与地球物理研究所
通讯作者Liang ChunTao
作者单位1.Chengdu Univ Technol, State Key Lab Geohazard Prevent & Geoenvironm Pro, Chengdu 610059, Sichuan, Peoples R China
2.Chengdu Univ Technol, Minist Educ, Key Lab Earth Explorat & Informat Technol, Chengdu 610059, Sichuan, Peoples R China
3.Shaanxi Earthquake Adm, Xian 710068, Shaanxi, Peoples R China
4.Chinese Acad Sci, Inst Geol & Geophys, Beijing 100029, Peoples R China
推荐引用方式
GB/T 7714
Liang ChunTao,Huang YanLing,Wang ChaoLiang,et al. Progress in the studies of the seismic gap between the 2008 Wenchuan and 2013 Lushan earthquakes[J]. CHINESE JOURNAL OF GEOPHYSICS-CHINESE EDITION,2018,61(5):1996-2010.
APA Liang ChunTao.,Huang YanLing.,Wang ChaoLiang.,Liu ZhiQiang.,Yang YiHai.,...&He FuJun.(2018).Progress in the studies of the seismic gap between the 2008 Wenchuan and 2013 Lushan earthquakes.CHINESE JOURNAL OF GEOPHYSICS-CHINESE EDITION,61(5),1996-2010.
MLA Liang ChunTao,et al."Progress in the studies of the seismic gap between the 2008 Wenchuan and 2013 Lushan earthquakes".CHINESE JOURNAL OF GEOPHYSICS-CHINESE EDITION 61.5(2018):1996-2010.

入库方式: OAI收割

来源:地质与地球物理研究所

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