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Formation and evolution of the Chinese marine basins

Science Bulletin 2007年第S1期 1-11页

作者： jia chengzao1, li benliang2, 3. zhang {3. li chuanxin1 1 research institute of petroleum Exploration and development, petrochina, beijing 100083. china 2 Resources and Information institute, {13. University of petroleum, beijing 102249, {13. 3.Central Laboratory of petroleum Geology research, research institute of petroleum Exploration and development, beijing 100083. china

There are plenty of petroleum resources in the Chinese marine basins, which will be the potential exploration regions of petroleum in the 21st century. The formation and evolution of the Chinese marine basins have mainly undergone two major tectonic epochs and five tectonic evolution stages. The first major tectonic epoch is the early Paleozoic plate divergence and drifting epoch during which the marine basins were formed, and the second one is the late Paleozoic plate convergence and collision epoch during which the pre-existent marine basins were superimposed and modified. The five tectonic evolution stages include: ① the drifting of micro-continental plates in Oceans and the formation of marine basins mainly filled with carbonate rocks during Proterozoic-Middle Carboniferous; ② the northward collage and convergence of continental plates and the {3. of the paralic sedimentary basins during Late Carboniferous-Middle Triassic; ③ the tectonically stabilized stage after the plate collage and the superimposition of lacustrine basins controlled by the inland subsidence during Late Triassic-Early Cretaceous; ④ the stage of the inland deformation and successive deep burial, uplifting, erosion or breakage of marine basins influenced by the plate tectonic activities of Neo-Tethys Ocean and the West Pacific developed in Late Cretaceous-Paleocene; ⑤ the stage of the foreland compression and basin-range coupling in the margin of the marine basins caused by the collision between India and Eurasia Plates and its long-distance effect since Neocene. The process of the tectonic evolution has controlled the petroleum geologic characteristics of Chinese marine basins, and a material foundation for the formation of oil and gas reservoirs has been built up via the formation of Paleozoic ma- rine basins, and the Mesozoic-Cenozoic tectonic superimposition and modification have controlled the key conditions of hydrocarbon accumulation and preservation. From the Late Proterozoic to

关键词： marine basin plate tectonics tectonics evolution petroleum exploration

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Formation and evolution of the Chinese marine basins

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Chinese Science Bulletin 2007年第A01期52卷 1-11页

作者： jia chengzao li {3. zhang xingyang li chuanxin research institute of petroleum Exploration and {3. PetroChina Beijing 100083 China Resources and Information institute China University of Petroleum Beijing 102249 China Central Laboratory of petroleum Geology research Research Institute of Petroleum Exploration and Development Beijing 100083 China

关键词：海洋盆地构造学石油资源

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