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《Geology in China》 2006-04
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Petrological structure, types and inhomogeneity of the lithosphere beneath continental China

QIU Rui-zhao1,2, LI Ting-dong 3,4, DENG Jin-fu5, ZHOU Su5, XIAO Qing-hui6, YE Tian-zha1, GENG Shu-fang2 (1. Development and Research Center, China Geological Survey, Beijing 100037, China; 2. Institute of Geology, Chinese Academy of Geological Sciences, Beijing 100037,, China; 3. Chinese Academy of Geological Sciences, Beijing 100037,, China; 4. College of Earth Sciences, Jilin University, Changchun 130061, Jilin, China; 5. China University of Geosciences, Beijing 100083, China; 6. Information Center, Ministry of Land and Resources, Beijing 100812, China)  
On the basis of the geological and geophysical characteristics of continental China, different lithospheric types in various regions are distinguished. In light of the petrological method, model of Earth's evolution and relationships between the seismic velocity and rock composition, eighteen petrological structure prisms corresponding with different lithospheric types have been set up. According to the dynamic properties, five types of lithosphere, i.e. cratonic, orogenic belt, rift, marginal oceanic crust and island―arc, are recognized in continental China. A petrological structure model of lithosphere beneath continental China is constructed and the inhomogeneous characteristics of the lithosphere beneath continental China are displayed for the first time.
【Fund】: 国土资源部科技专项计划项目(200010103);; 国家自然科学基金项目(NSFC402344048、No.40572063);; 中国地质调查局地质大调查项目(1212010561502、1212010561510、1212010561504);; 中国地质大学“岩石圈构造、深部过程及探测技术”教育部重点实验室开放课题(2003009、2003010)联合资助。
【CateGory Index】: P313.2
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