1985: MEAN STRESS FIELD IN TANGSHAN AFTERSHOCK AREA OBTAINED FROM FOCAL MECHANISM DATA BY FITTING SLIP DIRECTIONS. Acta Seismologica Sinica, 7(4): 349-362.
Citation: 1985: MEAN STRESS FIELD IN TANGSHAN AFTERSHOCK AREA OBTAINED FROM FOCAL MECHANISM DATA BY FITTING SLIP DIRECTIONS. Acta Seismologica Sinica, 7(4): 349-362.

MEAN STRESS FIELD IN TANGSHAN AFTERSHOCK AREA OBTAINED FROM FOCAL MECHANISM DATA BY FITTING SLIP DIRECTIONS

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  • Published Date: August 31, 2011
  • Alternatively taking each of the two nodal planes of focal mechanism solutions as the possible fault plane,the mean directions of principal stress axes and the relative magnitudes of intermediate principal stress in 3 sub-regions of the Tangshan aftershock area are estimated from 29 focal mechanism solutions by minimizing the angle between the calculated shear stress and the observed slip vector on every fault plane. The result indicates that the mean principal compressional stress axis in the Tangshan aftershock area is nearly horizontal,taking approximately the E-W direction. Comparing with the situation before the great 1976 Tangshan earthquake,this axis may have horizontally rotated about 30?clockwise. The stress axis directions inferred from the mean P,B and T axes of the composite fault plane solutions of aftershocks in the same 3 sub-regions are generally in agreement with the above result. A numerical test shows that,in some special case,there may appear a systematic deviation between the directions of the mean P,B and T axes and that of real principal stress axes in the crust.
  • [1] Yamakawa, (山川宜男),Stress field in focal regions, J. Phys. Earth, 19, 347——353, 1971.

    [2] 许忠淮,阎明,赵仲和,由多个小地震推断的华北地区构造应力场的方向,地震学报,5,268——279, 1983.

    [3] Etchecopar, A., G. Vasseur, and M. Daignieres, An inverse problem in microtectonics Eor the Determination of stress tensors from fault striation analysis, J. Struct. Geol., 3, 51——55, 1981.

    [4] Angelier, J., A. Tarantola, B. Valette and S. Manoussis, Inversion of field data in fault tectonics to obtaian the regional stress ——I. single phase fault populations: A new method of computing the stress tensor, Geophys. J. R. astr. Soc.,‘,,607——621, 1982.

    [5] 许忠淮,戈澎滇,用滑动方向拟合法反演富蕴地震断裂带应力场,地震学报,6, 395——404, 1984.

    [6] Ellsworth, W. L., and Xu Zhonghuai, Determination of the stress tensor from focal mechanism Data,EOS. Trans. Amen Geophys. Union., 61, 1117, 1980.

    [7] B.H.斯米尔诺夫著,高等数学教程,第三卷第一分册,第二章39节,人民教育出版社,1954年9月新1版。

    [8] 李钦祖,刁桂菩,戴英华,唐山地震序列的应力释放调整过程,地球物理学报,26, 224——236, 1983.

    [9] Wilkinson, J. H., The Algebraic Eigenvalue Problem, Chapter 2, Clarendon Press, Oxford, 1965.

    [1] Yamakawa, (山川宜男),Stress field in focal regions, J. Phys. Earth, 19, 347——353, 1971.

    [2] 许忠淮,阎明,赵仲和,由多个小地震推断的华北地区构造应力场的方向,地震学报,5,268——279, 1983.

    [3] Etchecopar, A., G. Vasseur, and M. Daignieres, An inverse problem in microtectonics Eor the Determination of stress tensors from fault striation analysis, J. Struct. Geol., 3, 51——55, 1981.

    [4] Angelier, J., A. Tarantola, B. Valette and S. Manoussis, Inversion of field data in fault tectonics to obtaian the regional stress ——I. single phase fault populations: A new method of computing the stress tensor, Geophys. J. R. astr. Soc.,‘,,607——621, 1982.

    [5] 许忠淮,戈澎滇,用滑动方向拟合法反演富蕴地震断裂带应力场,地震学报,6, 395——404, 1984.

    [6] Ellsworth, W. L., and Xu Zhonghuai, Determination of the stress tensor from focal mechanism Data,EOS. Trans. Amen Geophys. Union., 61, 1117, 1980.

    [7] B.H.斯米尔诺夫著,高等数学教程,第三卷第一分册,第二章39节,人民教育出版社,1954年9月新1版。

    [8] 李钦祖,刁桂菩,戴英华,唐山地震序列的应力释放调整过程,地球物理学报,26, 224——236, 1983.

    [9] Wilkinson, J. H., The Algebraic Eigenvalue Problem, Chapter 2, Clarendon Press, Oxford, 1965.
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