中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
The 2018M(W)7.5 Papua New Guinea Earthquake A Dissipative and Cascading Rupture Process

文献类型:期刊论文

作者Zhang, Xu; Feng, Wanpeng; Du, Hailin; Li, Lu; Wang, Shuai; Yi, Lei; Wang, Yongzhe
刊名GEOPHYSICAL RESEARCH LETTERS
出版日期2020-09-16
卷号47期号:17
ISSN号0094-8276
DOI10.1029/2020GL089271
英文摘要The 2018M(W)7.5 Papua New Guinea earthquake is the largest earthquake instrumentally recorded in the Papuan Fold Belt since 1900. Based on a combined analysis of backprojection imaging and finite-fault joint inversion, we determined a complex spatiotemporal rupture model of the mainshock. During the rupture process, three major asperities were ruptured successively with relatively low rupture velocities ranging from 1.9 to 2.3 km/s. The spatiotemporal evolution of the imparted Coulomb stress indicates that the rupture of the preceding asperity played an important role in triggering the delayed rupture of the adjacent asperity. Based on our rupture model, the upper bound of the radiation efficiency of this event is estimated to be 9.7-12.3%, a relatively low value, indicating that this earthquake is extremely dissipative. The high energy dissipation implies that the 2018M(W)7.5 Papua New Guinea earthquake may be controlled by the immature seismogenic environment.
源URL[http://ir.isl.ac.cn/handle/363002/33988]  
专题青海盐湖研究所_盐湖地质与环境实验室
中国科学院青海盐湖研究所
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GB/T 7714
Zhang, Xu,Feng, Wanpeng,Du, Hailin,et al. The 2018M(W)7.5 Papua New Guinea Earthquake A Dissipative and Cascading Rupture Process[J]. GEOPHYSICAL RESEARCH LETTERS,2020,47(17).
APA Zhang, Xu.,Feng, Wanpeng.,Du, Hailin.,Li, Lu.,Wang, Shuai.,...&Wang, Yongzhe.(2020).The 2018M(W)7.5 Papua New Guinea Earthquake A Dissipative and Cascading Rupture Process.GEOPHYSICAL RESEARCH LETTERS,47(17).
MLA Zhang, Xu,et al."The 2018M(W)7.5 Papua New Guinea Earthquake A Dissipative and Cascading Rupture Process".GEOPHYSICAL RESEARCH LETTERS 47.17(2020).

入库方式: OAI收割

来源:青海盐湖研究所

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