Slip Modeling of Large Earthquakes by Joint Inversion of W-Phase and Back-Projected Images

被引:1
作者
Peng, Yuyang [1 ]
Wang, Dun [1 ,2 ]
Takeuchi, Nozomu [3 ]
Rivera, Luis [4 ]
机构
[1] China Univ Geosci, Sch Earth Sci, Wuhan, Peoples R China
[2] China Univ Geosci, State Key Lab Geol Proc & Mineral Resources, Badong Natl Observat & Res Stn Geohazards, Wuhan, Peoples R China
[3] Univ Tokyo, Earthquake Res Inst, Tokyo, Japan
[4] Univ Strasbourg, CNRS, Inst Terre & Environement Strasbourg ITES, Strasbourg, France
基金
中国国家自然科学基金;
关键词
slip modeling; joint inversion; W-phase; back-projected images; 2015 GORKHA EARTHQUAKE; SOURCE PARAMETERS; NEPAL EARTHQUAKE; RUPTURE PROCESS; BACKPROJECTION; RADIATION; ROTATION; ILLAPEL; THRUST; ENERGY;
D O I
10.1029/2024JB029270
中图分类号
P3 [地球物理学]; P59 [地球化学];
学科分类号
0708 ; 070902 ;
摘要
We present a novel finite fault inversion algorithm that combines W-phase finite fault inversion with Image Deconvolution Back-Projection (IDBP) for the determination of coseismic slip models following large earthquakes. This integrated algorithm leverages the strengths of both methods, enabling rapid determination of moment tensor, slip distribution, and centroid location. The application of this integrated algorithm to the analysis of the 2015/04/25 Mw 7.8 Nepal and the 2013/01/05 Mw 7.5 Craig Alaska earthquakes yielded results closely aligned with detailed post-earthquake studies, highlighting the algorithm's accuracy and reliability. By overcoming inherent limitations of individual methods, it provides a comprehensive understanding of the earthquake source process. The algorithm's potential for automated implementation, requiring few parameters, enhances its suitability for near real-time earthquake analysis.
引用
收藏
页数:21
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