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《Chinese Journal of Geophysics》 2007-05
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Shear wave splitting in Himalaya

LIAO Wu-Lin~(1,2),DING Zhi-Feng~1,ZENG Rong-Sheng~1,ZHANG Hong~11 Institute of Geophysics,China Earthquake Administration,Beijing 100081,China2 Institute of Seismology,China Earthquake Administration,Wuhan 430071,China  
The records of 56 stations in Himalaya area were analyzed by using the method of minimizing the eigenvalue.Shear wave splitting was observed in thirty-nine stations of them.The average splitting time is about 0.8s.The parameters of splitting are not only different from south to north,but also different either side of the line joining the stations GAIG and T0040(AA′).To the west of the line,FPD(fast polarization direction) is mainly in the NWW or NW direction.To the east of it,FPD is in NNE to the south of MBT.FPD is NE or NEE in Lesser Himalaya and it becomes N-S or NEE in Tethys Himalaya.Comparing with other studies,we argue that the difference of splitting parameters between east and west is produced by lateral heterogeneous collision between Indian plate and Eurasia plate.The variation from south to north to the east of AA′ is produced by the complicated structure in this area.
【Fund】: 国家自然科学基金(40374036 40674044)资助
【CateGory Index】: P315
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