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《Journal of Changchun University of Science and Technology》 2003-02
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STRUCTURAL EVOLUTION FEATURES AND ITS SIGNIFICANCE OF HYDROCARBON EXPLORATION IN RELICT BASIN GROUP,EASTERN HEILONGJIANG PROVINCE

CAO Cheng-run 1 , ZHENG Qing-dao 2 (1.College of Earth Scien ces,Jilin University,Changchun 130061,China;2.Geomineral Exploration Bureau of Heilongjiang Province,Harbin 150036,China)  
Meso-Cenozoic basins controlled by Mudanjiang fault, Dun-Mi fau lt , Yi-Shu fault and Dahezhen fault are important basins of coal and oil-gas beari ng, NE China. Brittle-extension was the main process of forming basin group duri ng Meso-Cenozoic, so faulting or taphrogenesis sequences were well developed and depression (thermal subsidence) sequence was undeveloped in the basins. The stu dy of structural development, subsidence and extension process histories shows t hat the basin group universally went through early rapid subsidence (fault depre ssion) -basin attenuation and uplift denude-later intensive taphrogenes-sdeady attenuation or uplift denude. The process of forming basins and tectonic evoluti on can be divided into the four stages as Mesozoic epicontinental fault-depressi on all over the region (from later Jurassic to early Cretaceous), the first tect onic inversion(from later Cretaceous to Paleocene epoch),Cenozoic intracontinent al taphrogeny (from Eocene epoch to Oligocene epoch),the second tectonic inversi on(Neogene).The four stages reflect two main tectonic evolution cycles of the ba sin development. The tectonic evolution features of the basins resulted in dynam ic conditions for the multistage of hydrocarbon accumulation, on the other hand, transformed or destroyed the space-time distribution of dynamic and static stag e geological elements and their match relations.
【Fund】: 中国石油天然气集团公司“九五”重点科技攻关资助项目 (970 2 0 6 0 1)
【CateGory Index】: P618.13
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