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《Progress In Geophysics》 2003-02
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Geophysical discuss on extension to the east of boundary belt between Yangtze and Huanan Blocks

HAO Tian-yao1, LIU Jian-hua1, WANG Qian-shen1,SUH Mancheol2, DAI Ming-gang1 YAN Xiao-wei1(1. Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing 100029, China;2. Kongju National University,Kongju 314-701, Korea)JZ)  
It is known that Jiangshan-Shanxing, Qianshan-Yichun faults etc., are the boundary belt between Yangtze and Huanan blocks in East China area, but extension of this belt in sea areas was not so clear. In light with Free-air and Bouguer gravity data and tomography result in Yellow Sea and East China Sea, various information on faults were obtained after the processing (upward, arbitrary horizontal direction derivative, wavelet transform etc,.) and geophysical features of research region were analysis. It can be divided into different small areas according to geophysical feature differences. The geophysical evidences on the boundary belt between Yangtze and Huanan Blocks are shown after comprehensive analysis on gravity, magnetic, tomography result and geological information. It is believed that the boundary combine belt is possibly from Hangzhou Bay extending to round Nagasaki, Tsushima strait. It shows arc sharp to the north. The tomography result shows that geophysical evidences of the boundary belt can be found in the depth of upper mantle. Geophysical traces of this belt were not clear comparing with the boundary combine belt between Sino-korea and Yangtze Blocks. We believe that the tectonic movement of this combine belt became weaken after Caledonian movement.
【Fund】: 国家基础研究 973项目 (G2 0 0 0 0 467-0 1);; 国家自然科学基金项目 ( 4 0 0 740 2 1)联合资助 .
【CateGory Index】: P313
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