| Tectono-Sedimentary History of Southeastern Coast Region,China:a Synthesis |
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| 作者姓名： | Wu Chonglong Zhou Jiangyu Wang Gengfa Li ShaohuFaculty of Earth Resources China University of Geosciencex Wuhan Liu Pide Beijing High School Beijing |
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| 作者单位： | Wu Chonglong Zhou Jiangyu Wang Gengfa Li ShaohuFaculty of Earth Resources，China University of Geosciencex，Wuhan 430074Liu Pide Beijing 173 High School，Beijing 100008 |
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| 摘 要： | According to the ideas and concepts of systems dynamic of continent structure, using previous information related to the study area, combining analyses on orogenic belt, basin and magmatic rock, the present paper synthesizes the tectono-sedimentary development of southeastern coast region, China, with special emphasis on the mountain making, basining and magmafc activity. The tectonic evolution after Late Caledonian orogeny was dominated by alternating rifting and converging, subsiding and uplifting, mountain making and basining in central and southern parts of southeastern China and the adjacent regions to the east and west. Seventeen geologic events, nine events of plate or terrain convergence , and continental crust accretion, as well as eight events of intracontinental rifting and basin faulting , are closely related to the tectonic and sedimentary evolution of the study area. The accompanied intense and frequent sedimentation , folding , faulting , magmatism and ore-forming process allowed huge coal
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Tectono-Sedimentary History of Southeastern Coast Region, China : a Synthesis |
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| Wu Chonglong Zhou Jiangyu Wang Gengfa Li ShaohuFaculty of Earth Resources,China University of Geosciencex,Wuhan Liu Pide Beijing High School,Beijing .Tectono-Sedimentary History of Southeastern Coast Region,China:a Synthesis[J].Journal of China University of Geosciences,1995(2). |
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| Authors: | Wu Chonglong Zhou Jiangyu Wang Gengfa Li ShaohuFaculty of Earth Resources China University of Geosciencex Wuhan Liu Pide Beijing High School Beijing |
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| Institution: | Wu Chonglong Zhou Jiangyu Wang Gengfa Li ShaohuFaculty of Earth Resources,China University of Geosciencex,Wuhan 430074Liu Pide Beijing 173 High School,Beijing 100008 |
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| Abstract: | According to the ideas and concepts of systems dynamic of continent structure, using previous information related to the study area, combining analyses on orogenic belt, basin and magmatic rock, the present paper synthesizes the tectono - sedimentary development of southeastern coast region, China, with special emphasis on the mountain making, basining and magmatic activity. The tectonic evolution after Late Caledonian orogeny was dominated by alternating rifting and converging, subsiding and uplifting, mountain making and basining in central and southern parts of southeastern China and the adjacent regions to the east and west. Seventeen geologic events , nine events of plate or terrain convergence , and continental crust accretion , as well as eight events of intracontinental rifting and basin faulting , are closely related to the tectonic and sedimentary evolution of the study area . The accompanied intense and frequent sedimentation , folding , faulting , magmatism and ore- forming process allowed huge coal , multimetal and potential petroleum source rocks to form in local depressions throughout the Caledonian to Himalavan time . |
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| Keywords: | tectono - sedimentary history basin-orogen analysis Cathaysia subplate ac-tive continental margin Fujian - Guangdong superimposed basin southeastern coast of China |
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