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Volume 27 Issue 5
Sep 2016
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Yongge Wan, Shuzhong Sheng, Jichao Huang, Xiang Li, Xin Chen. The grid search algorithm of tectonic stress tensor based on focal mechanism data and its application in the boundary zone of China, Vietnam and Laos. Journal of Earth Science, 2016, 27(5): 777-785. doi: 10.1007/s12583-015-0649-1
Citation: Yongge Wan, Shuzhong Sheng, Jichao Huang, Xiang Li, Xin Chen. The grid search algorithm of tectonic stress tensor based on focal mechanism data and its application in the boundary zone of China, Vietnam and Laos. Journal of Earth Science, 2016, 27(5): 777-785. doi: 10.1007/s12583-015-0649-1

The grid search algorithm of tectonic stress tensor based on focal mechanism data and its application in the boundary zone of China, Vietnam and Laos

doi: 10.1007/s12583-015-0649-1
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  • Corresponding author: Yongge Wan, wanyg217217@vip.sina.com.cn
  • Received Date: 01 Sep 2014
  • Accepted Date: 11 Mar 2015
  • Publish Date: 01 Oct 2016
  • Stress field plays a key role in geodynamics. In this study, an algorithm to determine the stress tensor and its confidence range from focal mechanism data by using grid search method was proposed. The experiment uses artificial focal mechanism data which were generated by extensional, compression and strike-slip stress regime and different level of noise, shows that the precision of the estimated stress tensor based on this algorithm is greatly improved compared with traditional algorithms. This algorithm has three advantages: (1) The global optimal solution of the stress tensor is determined by fine grid search of 1º×1º×1º×0.01 and local minimum value is avoided; (2) precision of focal mechanism data can be considered, i.e., different weight of the focal mechanism data contributes differently to the process of determining stress tensor; (3) the confidence range of the determined stress tensor can be obtained by using F-test. We apply this algorithm in the boundary zone of China, Vietnam and Laos, and obtain the stress field with SSE-NNW compressive stress direction and NEE-SWW extensional stress direction. The stress ratio is 0.6, which shows that the eigen values of the stress tensor are nearly in arithmetic sequence. The stress field in this region is consistent with the left-lateral strike slip of the Dienbien-Lauangphrabang arc fault. The result will be helpful in studying the geological dynamic process in this region.

     

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