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Development characteristics of the fault system and its control on basin structure, Bodong Sag, East China

Development characteristics of the fault system and its control on basin structure, Bodong Sag, East China

作     者:Wu Zhiping Cheng Yanjun Yan Shiyong Su Wen Wang Xin Xu Changgui Zhou Xinhuai 

作者机构:China University of Petroleum Tianjin Technical Department CNOOC 

出 版 物:《Petroleum Science》 (石油科学(英文版))

年 卷 期:2013年第10卷第4期

页      面:450-457页

核心收录:

学科分类:0709[理学-地质学] 0819[工学-矿业工程] 0808[工学-电气工程] 081803[工学-地质工程] 07[理学] 08[工学] 0820[工学-石油与天然气工程] 070904[理学-构造地质学] 0707[理学-海洋科学] 0817[工学-化学工程与技术] 0818[工学-地质资源与地质工程] 0708[理学-地球物理学] 0807[工学-动力工程及工程热物理] 0815[工学-水利工程] 0816[工学-测绘科学与技术] 0827[工学-核科学与技术] 0703[理学-化学] 0813[工学-建筑学] 0825[工学-航空宇航科学与技术] 0704[理学-天文学] 0814[工学-土木工程] 

主  题:Fault system basin structure Bodong area 

摘      要:The Bodong Sag,located in the Bohai Sea,offshore China,is one of the most petroliferous basins in *** on three dimensional seismic reflection data and time slice data,we analyze the fault system of the Bodong area in detail,establish the fault structure pattern of different types and summarize the distribution of the fault *** is concluded that the development characteristics of the Cenozoic fault system are in accordance with the dextral stress field of the Tanlu Fault,which displayed a brush structure with NNE strike-slip faults as its principal faults,NE-trending extensional faults as secondary faults and EW-trending faults as minor *** can be divided into (1) strike-slip type,(2) extensional type,(3) strike-slip extensional type and (4) extensional strike-slip *** spatial structures of different faults have obvious differences because of the fault properties and activity *** fault system at different stages shows tremendous differences because of the transition of the Tanlu Fault from sinistral strike-slip to dextral strike-slip,the transition between extension and strike-slip,and the transition from mantle upwelling to thermal *** to the controlling effect of faults on basin structure,the Cenozoic basin experienced four evolutionary stages,(a) transition stage from sinistral strike-slip to dextral strike-slip,(b) strike-slip extensional faulted stage,(c) extensional strike-slip faulted stage and (d) strike-slip depression *** identification of temporal and spatial differences of faults could be used as a significant guideline for oil and gas exploration in the Bodong area.

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