Abstract:SUMMARY
Based on 43 Harvard CMT solutions in Yunnan region, GPS observations from 1999 to 2004 by ChinaCrustal Movement Observatory Network, and results from SKS splitting and Pn fast wave anisotropy, we obtained the average directions of principle stress fields at different depths by average angle method. Then we further analyzed the coupling difference between geodynamic parameters in different tectonic blocks. Then we built five three-dimensional finite element models to simulate the crustal velocity field … Show more
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