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《Chinese Journal of Geophysics》 2006-01
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A study on SKS splitting beneath the Yunnan region

CHANG Li-Jun,WANG Chun-Yong,DING Zhi-FengInstitute of Geophysics, China Earthquake Administration, Beijing 100081, China  
SKS shear waves recorded at 47 stations, which are located in Yunnan and involve Yunnan digital seismograph network, Yunnan temporary seismometer arrays, and China National Digital Seismograph Network (CNDSN), are used to analyze the direction and extent of seismic anisotropy. Furthermore, some problems related to the dynamics of the Qinghai_Tibetan plateau are discussed. It is demonstrated that delay times vary from 0.58 to 1.88s and fast wave polarization directions are present at stations with nearly N-S in northern Yunnan and gradually rotate to W-E in southern Yunnan. The shear wave splitting is mainly due to the anisotropy in the upper mantle whose thickness is between 67km and 216km. It is possible that the collision of the India and Eurasia plates resulted in not only crustal thickening and subsequently the E-W extension beneath the Qinghai_Tibetan plateau, but also mantle material flow southeastward.
【Fund】: 国家自然科学基金项目(40334041)资助.
【CateGory Index】: P315.31
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