Inversion of stresses from polyphase fault/slip data with high or low diversity: An updated version of INVSFS

被引:3
|
作者
Shan, Yehua [1 ]
Tian, Ye [1 ]
Xiao, Wenjiao [2 ]
机构
[1] Chinese Acad Sci, Lab Marginal Sea Geol, Guangzhou Inst Geochem, Guangzhou 510640, Peoples R China
[2] Chinese Acad Sci, Inst Geol & Geophys, State Key Lab Lithospher Evolut, Beijing 100029, Peoples R China
基金
中国国家自然科学基金;
关键词
fault/slip data; Polyphase; Low diversity; Sigma space; Stress inversion; 1999; CHI-CHI; SURFACE RUPTURE; SLIP DATA; EARTHQUAKE; SEPARATION;
D O I
10.1016/j.cageo.2010.11.002
中图分类号
TP39 [计算机的应用];
学科分类号
081203 ; 0835 ;
摘要
Fault/slip data with low diversity show limited range in orientation, and their equations, according to the Wallace-Bott hypothesis often give rise to an unstable stress solution. It is necessary in this case to introduce some auxiliary constraint(s), so as to make a stable stress solution from these equations. A new method for inverting stress from polyphase fault/slip data with low diversity but having all or a majority of newly formed faults in each subset is developed in this paper. It combines a weak criterion that favors the newly formed faults, together with the Wallace-Bott hypothesis or the strong criterion. Both criteria are solved for stresses using the Fuzzy C-lines clustering analysis technique. This permits the updating of the INVSFS code (Li et al., 2005). Two artificial sets of polyphase fault/slip data with high and low diversity are chosen to demonstrate the performance of the updated version. (C) 2010 Elsevier Ltd. All rights reserved.
引用
收藏
页码:1045 / 1053
页数:9
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