Abstract
Genetic algorithm-finite element method (GA-FEM) is applied to the study of tectonic stress field of part of East Asia area. From the observed stress distribution, 2-D elastic plane stress inversion is made to deduce the boundary forces and investigate controlling factors. It is suggested that the continent-continent collision is the dominant factor controlling the Chinese tectonic stress field. The ocean-continent convergence along the subduction zone is an important factor. There exists tensile boundary force along the marginal sea.
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References
An M J and Shi Y L, 1996. Dynamic genetic algorithms inversion of earthquake focal mechanism from P waves first motions. Earthquake Research in China, 12(4): 394–402 (in Chinese)
An M J, Shi Y L and Li F Q, 1997. Preliminary researches for genetic algorithm-finite element method (GA-FEM) inversion with ideal model. In: Collected Works of Crustal Structure and Crustal Stress (10). Beijing: Seismological Press, 164–171 (in Chinese)
Angelier L, 1990. Foreword—geodynamics of the eastern Eurasian margin. Tectonophysics, 183(1–4): VII-X
Aubouin J, 1990. The west Pacific geodynamic model. Tectonophysics, 183(1–4): 1–7
Chinese Seismic Zoning Committee, SSB, 1991. The Figures and Specification of Earthquake Focal Mechanism In and Near China. Beijing: Seismological Press, 7–17 (in Chinese)
DeMets C, Gordon G R, Argus D F, et al., 1990. Current plate motions. Geophys J Int, 101: 425–478
Dziewonski A M and Anderson D L, 1981. Preliminary reference earth model. Phys Earth Planet Int, 25: 297–356
Eguchi T, 1983. Tectonics stress field in East Eurasia. Phys Earth Plane Interi, 33: 318–327
Fu R S and Huang J H, 1989. Lithospheric stress field and its deep dynamic background. In: Geophysics Advance in China in 1980s. Beijing: Science Journal Press, 326–336 (in Chinese)
Goldberg D E, 1986. Genetic Algorithms In Search, Optimization And Machine Learning. Reading: Anddision-Wesley, Pub., 412
Letouzey J and Kimura M, 1986. The Okinawa trough: genesis of a back-arc basin developing along a continental margin. Tectonophysics, 125(1–3): 209–230
Li F Q and Liu G X, 1986. The present state of stress field in China and the related problems. Acta Seismologica Sinica, 8(2): 156–171(in Chinese)
Li F Q, 1992. Comparison of the results obtained from different techniques such as overcoring, hydrofracturing, breakouts and focal mechanism solutions. Acta Seismologica Sinica, 14(2): 149–155 (in Chinese)
Li F Q, Li Y M, Wang E F, et al., 1984. Experiments of in-situ stress measurements using stress relief and hydraulic fracturing techniques. In: Collected Works of Crustal Stress Research. Beijing: Seismological Press, 9–17 (in Chinese)
Li F Q, Zhai Q S, Bi S X, et al., 1986. In-situ stress measurement by hydraulic fracturing and preliminary results. Acta Seismologica Sinica, 8(4): 431–438 (in Chinese)
Li Z Y, Li X G and Ran Y K, 1989. Neotectonics. In: Lithospheric Dynamics Atlas of China. Beijing: China Cartographic Publishing House, 16pp (in Chinese)
Liu H S, 1978. Mantle convection pattern and subcrustal stress field under Asia. Phys of Earth Planet Inter, 16: 247–256
Owen D R J and Hinton E, 1980. Finite Elements in Plasticity — Theory and Practice. New York: Pineridge Press Ltd., 157–269
Shi Y L and Jin W, 1985. Genetic algorithm of the earth interior inversion using surface wave dispersion. Acta Geophysica Sinica, 38(2): 189–198 (in Chinese)
Shi Y L and Wang Q Y, 1993. The roll-back of subduction zone and the back-arc extension. Acta Geophysica Sinica, 36(1): 37–43 (in Chinese)
Shi Y L and Wang Q Y, 1994. Analysis of the mechanism of oblique subduction plate boundary deformation. Acta Geophysica Sinica, 37(5): 606–612 (in Chinese)
Shi Y L, 1992. Genetic algorithm and its application on geophysics. Acta Geophysica Sinica, 35(Suppl): 367–371 (in Chinese)
Wang R, 1983. A short note on the inversion of tectonic stress fields. Tectonophysics, 100(1–3): 405–411
Wang R and Liang H H, 1985. The east Asia stress field inversion using superposition method. In: Collected Works of International Geoscience Exchange (2). Beijing: Geology Press, 29–36 (in Chinese)
Wang S Y and Chen P S, 1980. Numerical modeling of recent tectonic stress field in and near China. Acta Geophysica Sinica, 23(1): 35–45 (in Chinese)
Wang S Y, Xu Z H, Yu Y X, et al., 1996. The research on the plate reaction force in and near China. Acta Geophysica Sinica, 39(6): 764–771 (in Chinese)
Xu Z H, Wang X Y, Gao A J, et al., 1994. The renew determination and review of earthquake focal mechanism in China. In: Zang S X (in-chief-editor), Annual of the Chinese Geophysical Society. Beijing: Seismological Press, 133
Xu Z H, Wang S Y and Yu Y X, 1992. The inversion of plate boundary reaction forces using observed stress azimuth by finite element method. Acta Seismologica Sinica, 14(4): 446–455 (in Chinese)
Yu Y X, Xu Z H and Wang S Y, 1989. One of explanations to the overall feature of the crustal stress field in China’s continent. In: Geophysics Advance in China in 1980s. Beijing: Science Journal Press, 284–292 (in Chinese)
Zang S X and Ning J Y, 1996. The research on and the dynamics meaning of west pacific subduction zone. Acta Geophysica Sinica, 39(2): 188–202 (in Chinese)
Zang S X, Ning J Y, Liu B C, et al., 1989. The interaction of plates around China and its effect on the stress field in China—Part I, the influence of Pacific plate and Philippine sea plate. In: Geophysics Advance in China in 1980s. Beijing: Science Journal Press, 293–306 (in Chinese)
Zang S X, Wu Z L, Ning J Y, et al., 1992. The interaction of plates around China and its effect on the stress field in China—Part II, the influence of India plate. Acta Geophysica Sinica, 35(3): 428–440 (in Chinese)
Zoback M L, 1992. First- and second-order patterns of stress in lithosphere: The world stress map project. J Geophy R, 97(B8): 11704–11728
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This study is supported by the National Natural Science Foundation of China (NSFC).
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An, MJ., Shi, YL. & Li, FQ. Genetic algorithm-finite element method inversion of the factors determining the recent tectonic stress field of part of East Asia area. Acta Seimol. Sin. 11, 265–272 (1998). https://doi.org/10.1007/s11589-998-0034-6
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DOI: https://doi.org/10.1007/s11589-998-0034-6