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《Chinese Journal of Geophysics》 2005-05
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Using surface wave and receiver function to jointly inverse the crust-mantle velocity structure in the West Yunnan area

HU Jia-Fu 1,ZHU Xiong-Guan 1,XIA Jing-Yu 1,CHEN Yun 21 Geophysics Department of Yunnan University, Kunming 650091, China2 Institute of Geology and Geophysics of Chinese Academy of Sciences, Beijing 100029, China  
Because surface wave dispersion is well sensitive to S wave velocity and receiver function is sensitive to interface depth, respectively, we use surface wave and receiver function data to make a joint inversion to probe the crust_mantle velocity structure beneath western Yunnan Province. We apply the technique of matched_filter frequency_time analysis to process long_period surface wave data covering western Yunnnan and obtain the surface wave group velocity dispersion in the period range 10.5~105.0s. Then we employ the grid inversion method to extract pure path dispersion in the grid 1°×1° in the study area. Using the teleseismic broadband records of western Yunnan and the deconvolution method, we obtain the teleseismic P wave receiver function beneath the stations. Combining the information of surface wave pure path dispersion and the receiver function data, we perform a joint inversion by means of the damped least_squares method to determine the crust_mantle velocity structure beneath western Yunnan. The result shows that taking the Red River Fault as the boundary, the structures of the crust and mantle on its both sides are notably different. On the west side of the fault there is a low_velocity layer of ~10km thickness at depth ~20km, while this layer is not apparent on the east side of the fault. Beneath the Wanding and Cangyuan areas, which are geologically located in the Yunnan_Myanmar_Thailand block, the upper mantle has a relatively low velocity. Another low_velocity layer of the upper mantle appears below the Kangdian palaeo_uplift in the Mid_Yunnan block. It seems that these two low_velocity layers of the mantle are associated with the distributions of high heat flow and major earthquakes.
【Fund】: 国家自然科学基金(40274030);; 云南省自然科学基金(2002D0007M)资助.
【CateGory Index】: P315;P542.5
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