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《Chinese Journal of Geophysics》 2003-01
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STUDY ON CHARACTERS OF TWO PHASES STRUCTURAL EVOLUTION AT THE LIAOHE BASIN,CHINA DURING PALEOGENE TIMES

SHAN JIAZENG1 SUN HONGJUN2 XIAO QIANHUA2 WANG DAOJING1 XU KUN2 LIU XIAOFENG2 SHEN DAYUAN2 SUN SUQING2 1 Institute of Geology and Geophysics,Chinese Academy of Sciences,Beijing 100029,China 2 Exploration and Development Research Institute of Liaohe Oil Field.Panjin 124010.China  
New geophysical evidence and the results of the modeling experiment indicate that the structural history of the Liaohe basin,China during the Paleogene times consists of two phases,a continental rift phase and a dextral strike-slip phase.The continental rift is driven by extensional stresses from upwelling of the mantle during the Fangshenpao and Shahejie phases of Paleocene and Eocene,Paleogene times(Ef-Esl,about 63.0~37.0Ma).The dextral strike-slip movement occurred during the Dongying phase of Oligocene,Paleogene times(Ed,about 36.9~24.5Ma).Two phases of the structural movement lead to forming and evolution of complex fault system in the Liaohe basin.It is suggested that dextral strike-slip movement of post-rift reactivated older extensional faults and produced new faults.On the basis of results from modeling experiments and analysis of geophysical information,the displacement magnitudes caused by dextral strike movement during the Dongying phase of Paleogene times(Ed)is about 4~8km.New studies prove that complex fault systems of the Liaohe basin are not only strongly controlled by older extensional stresses,but also influenced by younger dextral strike-slip movement.Two phase structural movement resulted in oil and gas migration and accululation in this area.
【Fund】: 国家自然科学基金项目 (49472 1 39);; 辽河油田资助项目 (LH一 2 4 3) .
【CateGory Index】: P542
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