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《Chinese Journal of Geophysics》 2001-05
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THE RAYLEIGH WAVE DISPERSION AND THREE DIMENSIONAL VELOCITY STRUCTURE IN CONTINENT AND ITS MARGIN OF SOUTHEAST CHINA

WTTENG JWT6IWT-WWT6ENWT,ZHANG ZWT6HONGWT-JWT6IE,WTWANG GWT6UANGWT-JWT6IEWTWT6BX(Institute of Geology and Geophysics,Chinese Academy of Sciences,Beijing 100101,China)WTHU JWT6IAWT-FWT6UWT6BX(Yunnan University,Yunnan 650091,China)  
HTWTIn this study,the dispersion of Rayleigh waves crossing Southeast China and its continental margin is determined by applying the (Matched-filter frequency-time analysis) technique to CDSN mid-long period data. The technique improves the resolution of dispersion measurement over a broader period range with reduced systematic errors. An improved grid dispersion inversion is proposed to extract pure-path dispersion curves in 4°×4° grid from the mixed path dispersion data. On the basis of the grid dispersion inversion,we use Harkrider surfer Wave inversion program to study the three dimension shear wave velocity structure to depth of 200km. A detailed description on the lateral heterogeneity in the crust and upper mantle of Southeast China is provided. The results show that:1. The depth of Moho is generally 30_40km in continent region of Southeast China and 25_28km in its continental margin. The crustal thickness is thin from west,and the features of regional division are quite clear. 2. The depth of the low velocity layer in the upper mantle is 60_150km in continent of southeast China. Distribution of deep faults and deep internal processes has something to do with the great variational amplitude for the lower velocity layer in the upper mantle. 3. The Southeast margin of China is a transition belt between continent and Sea. Its characteristics are shown that there is a low velocity zone and the depth of the Moho is shallow. The undulate shape of deep interface of the mantle makes clear,moreover,its cupping between deep and shallow and structure is inhomogeneity. WTHZHTH
【Fund】: 中国科学院重点项目 (KZ95 2 -S1 -41 0 ) ;; 国家自然科学基金资助项目 (4 0 0 740 2 0 )
【CateGory Index】: P541
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