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《Geology in China》 2009-05
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A discussion on the tectonic framework of Chinese mainland

GE Xiao-hong1,2,MA Wen-pu2,LIU Jun-lai2,REN Shou-mai3,LIU Yong-jiang1,YUAN Si-hua4,WANG Min-pei2(1.College of Earth Sciences,Jilin University,Changchun 130061,Jilin,China;2.School of Earth Sciences and Resources,China University of Geosciences,Beijing 100083,China;3.Strategic Research Center of Oil & Gas Resources,Ministry of Land and Resources,Beijing 100034,China;4.Institute of Geology,Chinese Academy of Geological Sciences,Beijing 100037,China)  
A new way of thinking is opened up by the generation of the continental dynamic theory and its application to the study of tectonics of Chinese mainland.The Precambrian basement and the South China-Indo-China stratigraphic framework are regarded as the essential factors in the outlining and subdivision of the tectonic framework of Chinese mainland.Nevertheless,it is also necessary to carry out studies of important intracontinental deformation structures such as large scale strike-slip faulting,nappe structures and extrusion tectonics as well as their influence on the tectonic framework formed during and before the Indo-China stage.The properties of the pre-Indo-China tectonic units should therefore be reevaluated through tectonic reconstruction.A study of the tectonic reconstruction of Western China has led the authors to believe that Alxa,Mid-Qilian,Qaidam and northern Qiangtang blocks as well as Tarim plate belong to a unified craton of Xiyu Plate,while Kunlun-Qilian-Qinling ocean plate is not existent.The Early Paleozoic Maijia'er-North Qilian small ocean basin and Late Paleozoic East Kunlun-Animaqing-Jinshajiang faulted depression ocean basin might have resulted from the wedging action of the ridge of Paleo-Tethys ocean,and the environment must have been quite similar to that of the present Red Sea-Aden gulf.This paper deals with some of the basic controversies concerning the tectonic framework of China and its adjacent areas,with an investigation of the tectonic evolution of Chinese mainland in such aspects as the properties and ascription of Alxa and northern Qiangtang blocks,the confirmation of the existence of Western China plate,the tectonic subdivision of the North Asian tectonic domain in China,the Late Jurassic and Early Cretaceous intracontinental deformation and Central Asia extrusion tectonics,the subdivision of Sino-Korean plate and Yangtze-South China plate and the ascription of the southern North Yellow sea and Korean peninsula.
【Fund】: 国家自然科学基金(49772157和40272099)资助
【CateGory Index】: P542
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1 Wei Dan~(a,b),Xian-Hua Li ~(a,c,*),Jinghui Guo~a,Yu Liu~a,Xuan-Ce Wang~(a,d) a State Key Laboratory of Lithospheric Evolution,Institute of Geology and Geophysics,Chinese Academy of Sciences,Beijing 100029,China b Graduate School of Chinese Academy of Sciences,Beijing 100039,China c State Key Laboratory of Geological Processes and Mineral Resources.China University of Geosciences.Wuhan.Hubei 430074.China d The Institute for Geoscience Research,Department of Applied Geology,Curtin University of Technology,Perth,WA 6845,Australia;Paleoproterozoic evolution of the eastern Alxa Block,westernmost North China:Evidence from in situ zircon U-Pb dating and Hf-0 isotopes[A];[C];2013
2 CHU ShaoXiong,LIU JianMing,XU JiuHua,WEI Hao,CHAI Hui and TONG KuangYin 1.Key Laboratory of Mineral Resources,Institute of Geology and Geophysics,CAS,Beijing 100029,China 2.Resource Engineering Department,University of Science and Technology Beijing,Beijing 100083,China 3.School of Earth Sciences and Resources,China University of Geosciences,Beijing 100083,China 4.Heilongjiang Heilong Mining Group Co.,Ltd,Harbin 150090,China;Zircon U-Pb dating,petrogenesis and tectonic significance of the granodiorite in the Sankuanggou skarn Fe-Cu deposit,Heilongjiang Province[A];[C];2013
3 Jianyun Feng~(a,b),Wenjiao Xiao~(a,c,*),Brian Windley~d,Chunming Han~(a,c), Bo Wan~a,Ji'en Zhang~a,Songjian Ao~a,Zhiyong Zhang~a,Lina Lin~(a,b) a State Key Laboratory of Lithospheric Evolution,Institute of Geology and Geophysics,Chinese Academy of Sciences,Beijing 100029,China b Graduate University of Chinese Academy of Sciences,Beijing 100049,China c Xinjiang Research Center for Mineral Resources,Xinjiang Institute of Ecology and Geography,Chinese Academy of Sciences,Urumqi 830011,China d Department of Geology,University of Leicester,Leicester LE1 7RH,UK;Field geology,geochronology and geochemistry of mafic-ultramafic rocks from Alxa,China:Implications for Late Permian accretionary tectonics in the southern Altaids[A];[C];2014
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3 Huo Fuchen Cao Jingxuan Dong YanshengGu Qichang Yan Zhiqiang (The Bureau of Geology and Mineral of Ningxia);THE DIVISION, CORRELATION, METAMORPHISM AND MINERALIZATION FEATURES OF THE LOWER AND MIDDLE PRECAMBRIAN IN THE HELANSHAN MOUNTAIN -ALASHAN REGION, CHINA[J];;1987-01
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10 LI Cai, WANG Tian_wu, YANG De_ming, YANG Ri_hong (College of Earth Sciences, Jilin University, Changchun 130026,China) \;;THE LITHOLOGICAL COMPOSITION AND TECTONIC EVOLUTION OF QIANGTANG CENTRAL UPLIFT REGION,TIBET[J];Journal of Changchun University of Science and Technology;2001-01
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1 Sun Xiaomeng Zhang Haiqing (China University of Geosciences, Beijing 100083) Yao Wengui (Changchun College of Geology, Changchun 130061);SEVERAL PROBLEMS IN STUDYING THE AGE OF OPHIOLITES AND OPHIOLITIC MELANGES[A];[C];1996
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