Modern tectonic stress field in the Chinese mainland inverted from focal mechanism solutions
Author:
Publisher
Springer Science and Business Media LLC
Subject
Geophysics,Geotechnical Engineering and Engineering Geology
Link
http://link.springer.com/content/pdf/10.1007/s11589-999-0078-2.pdf
Reference8 articles.
1. Angelier J. 1979. Determination of the mean principal directions of stresses for a given population. Tectonophysics, 56: 17–26
2. Editorial Board of China Earthquake Yearbook. 1983–1994. China Earthquake YearBook. Beijing: Seismological Press
3. Du X X, Zhang H L, Lu X L, et al. 1997. Research on inversion of average stress field by genetic algorithms. Acta Seismologica Sinica, 10(2): 261–265
4. Ellsworth W L. 1981. A general theory for determining the state of stress in the earth from fault slip measurements. Terra Congnita, 2(2): 170–171
5. Gephart J W, Forsyth D W. 1984. An improved method for determining the regional stress tensor using earthquake focal mechanism data: application to San Fernando earthquake sequence. J Geophys Res, 89(B11): 9 305–9 320
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1. Contemporary tectonic stress field in China;Earthquake Science;2010-08
2. Inversion of stress field in Guangdong and its adjacent area;Acta Seismologica Sinica;2008-01
3. An interfacial mechanical model for the analysis of earthquake;Acta Seismologica Sinica;2000-09
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