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《Acta Geologica Sinica》 2010-06
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Fine Structure of the Continental Lithosphere Circle Revealed by Deep Seismic Reflection Profile

WANG Haiyan1,2), GAO Rui1,2), LU Zhanwu1,2), LI Qiusheng1,2), KUANG Zhaoyang2,3), LIU Jinkai2,3), HOU Hesheng1,2), FENG Shaoying1,2,4), XIONG Xiaosong1,2), LI Wenhui1,2), DENG Gong1,2)1) Lithosphere Research Centre, Institute of Geology, CAGS, Beijing, 100037;2) Key Laboratory of Earth Probe and Geodynamics, CAGS, Beijing, 100037;3) No.6 Geophysical Prospecting Team, China Petroleum & Chemical Corporation, Nanjing, 210011;4) Geophysical Prospecting Center, China Earthquake Administration, Zhengzhou, 450002  
Deep seismic reflection has currently been recognized as an effective technological approach in probing fine structure of lithosphere and solving the deep geological problems. Since the 1970s, the western countries with America as a leading one and China have successively carried out deep seismic reflection exploration program. The technology of this kind has been widely used to disclose the formation and evolution of lithosphere in basins and the orogenic belts, geodynamics processes, and has been applied in prospective evaluation of oil and gas resources, mineral resources exploration and other fields. A large amount of results have been achieved. The development of deep seismic reflection technique and its part of the applications example are described briefly in this paper.
【Fund】: 国家专项“深部探测技术与实验研究”(编号SinoProbe-02);; 国家自然科学基金重点项目(编号40830316)、国家自然科学青年金项目(编号40604010);; 科技部国际合作重点项目(编号2006DFA21340);; 国土资源部地质调查项目(编号1212010711813);; 基本科研业务费项目(编号J0803)联合资助成果
【CateGory Index】: P631.4
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