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The 2018M(W)7.5 Papua New Guinea Earthquake A Dissipative and Cascading Rupture Process
Zhang, Xu; Feng, Wanpeng; Du, Hailin; Li, Lu; Wang, Shuai; Yi, Lei; Wang, Yongzhe
FirstAuthorZhang, Xu
2020-09-16
Source PublicationGEOPHYSICAL RESEARCH LETTERS
ISSN0094-8276
Volume47Issue:17
AbstractThe 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.
DOI10.1029/2020GL089271
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Document Type期刊论文
Identifierhttp://ir.isl.ac.cn/handle/363002/33988
Collection盐湖地质与环境实验室
中国科学院青海盐湖研究所
Recommended Citation
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).
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