CCPortal
DOI10.1002/2013GL056876
Rupture history of the 2013 M-w 6.6 Lushan earthquake constrained with local strong motion and teleseismic body and surface waves
Hao, Jinlai; Ji, Chen; Wang, Weimin; Yao, Zhenxing
通讯作者Ji, C (通讯作者)
发表日期2013
ISSN0094-8276
EISSN1944-8007
起始页码5371
结束页码5376
卷号40期号:20
英文摘要The rupture history of the 20 April 2013 M-w 6.6 Lushan (China) earthquake is constrained by inverting waveforms of local strong motion, teleseismic broadband body waves, and long-period surface waves. This earthquake ruptured a blind thrust fault oriented N210 degrees E (along the Longmenshan fault zone) and dipping 40 degrees to the NW. The inverted slip distribution is heterogeneous, dominated by a slip patch with a roughly right triangular shape, which spans a depth range of 5-20 km and accounts for two thirds of the total seismic moment (8.9 x 10(18) N m). The rupture initiated roughly at the middle of the triangle's hypotenuse and, during the first 4 s, propagated mainly in along-strike and downdip directions, toward a peak slip of 1.2 m. Despite a large number of fatalities and economic loss, the estimated static and apparent stress drops of the Lushan earthquake are 1.5 MPa and 0.35 MPa, considerably low with respect to other similar intraplate earthquakes.
关键词SLIP HISTORYCALIFORNIAHAZARDENERGY
语种英语
WOS研究方向Geology
WOS类目Geosciences, Multidisciplinary
WOS记录号WOS:000330514200008
来源期刊GEOPHYSICAL RESEARCH LETTERS
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/258158
推荐引用方式
GB/T 7714
Hao, Jinlai,Ji, Chen,Wang, Weimin,et al. Rupture history of the 2013 M-w 6.6 Lushan earthquake constrained with local strong motion and teleseismic body and surface waves[J]. 中国科学院青藏高原研究所,2013,40(20).
APA Hao, Jinlai,Ji, Chen,Wang, Weimin,&Yao, Zhenxing.(2013).Rupture history of the 2013 M-w 6.6 Lushan earthquake constrained with local strong motion and teleseismic body and surface waves.GEOPHYSICAL RESEARCH LETTERS,40(20).
MLA Hao, Jinlai,et al."Rupture history of the 2013 M-w 6.6 Lushan earthquake constrained with local strong motion and teleseismic body and surface waves".GEOPHYSICAL RESEARCH LETTERS 40.20(2013).
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