中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
Gravity changes associated with the m(s)8. 0 wenchuan earthquake detected by grace

文献类型:期刊论文

作者Wang Wu-Xing1,2; Shi Yao-Lin2; Gu Guo-Hua1; Zhang Jing1; Chen Shi3
刊名Chinese journal of geophysics-chinese edition
出版日期2010-08-01
卷号53期号:8页码:1767-1777
关键词Wenchuan earthquake Sumatra earthquake Grace satellites Change in gravity Gps Displacement
ISSN号0001-5733
DOI10.3969/j.issn.0001-5733.2010.08.002
通讯作者Wang wu-xing(bkwwx@seis.ac.cn)
英文摘要Time variable changes in gravity field on and around chinese mainland before and after the wenchuan m(s)8. 0 earthquake are obtained from the grace satellite gravity data. time series of gravity changes at typical locations are also obtained. at the same time, time series of displacements at gps fiducial stations of wush, lhas, kunm and luzh are obtained in the regional reference frame. results from grace indicate that after the sumatra earthquake along the himalaya arc the satellite gravity showed rapid decrease, particularly during the period of 2006 to 2008 the decrease in gravity was significant; while along the northwestern boundary of the xiyu block there was also significant post seismic decrease in gravity. and along the northern and eastern boundaries of the tibetan plateau there appeared an arc along the tectonic boundary with significant gravity increase in 2007. but in 2008 there was also significant increase in gravity in the southern and middle segments of the north-south seismic belt. this trend in gravity variations after the sumatra earthquake changed only after the wenchuan earthquake. displacements at 4 gps stations recorded coseismic signals of the great sumatra earthquake, and then the horizontal displacement vectors at wush, lhas and kunm showed significant changes in their general trend until the occurrence of the wenchuan m(s)8. 0 earthquake. the changes in the density of the ground mass in the tibetan plateau and the surrounding areas as revealed by the grace satellites have provided new observation approach and data for the explanation of the dynamic mechanism of the wenchuan earthquake. a preliminary explanation and discussion on the characteristics of the time variable changes in the gravity field observed by grace and the dynamic mechanism of the wenchuan earthquake are presented in this paper by combining the features of regional tectonic movements and displacements of gps observations.
WOS关键词DEFORMATION ; CHINA ; ZONE
WOS研究方向Geochemistry & Geophysics
WOS类目Geochemistry & Geophysics
语种英语
WOS记录号WOS:000281331800002
出版者SCIENCE PRESS
URI标识http://www.irgrid.ac.cn/handle/1471x/2411434
专题中国科学院大学
通讯作者Wang Wu-Xing
作者单位1.China Earthquake Adm, Inst Earthquake Sci, Beijing 100036, Peoples R China
2.Chinese Acad Sci, Grad Univ, Lab Computat Geodynam, Beijing 100049, Peoples R China
3.China Earthquake Adm, Inst Geophys, Beijing 100081, Peoples R China
推荐引用方式
GB/T 7714
Wang Wu-Xing,Shi Yao-Lin,Gu Guo-Hua,et al. Gravity changes associated with the m(s)8. 0 wenchuan earthquake detected by grace[J]. Chinese journal of geophysics-chinese edition,2010,53(8):1767-1777.
APA Wang Wu-Xing,Shi Yao-Lin,Gu Guo-Hua,Zhang Jing,&Chen Shi.(2010).Gravity changes associated with the m(s)8. 0 wenchuan earthquake detected by grace.Chinese journal of geophysics-chinese edition,53(8),1767-1777.
MLA Wang Wu-Xing,et al."Gravity changes associated with the m(s)8. 0 wenchuan earthquake detected by grace".Chinese journal of geophysics-chinese edition 53.8(2010):1767-1777.

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来源:中国科学院大学

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