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《MARINE GEOLOGY & QUATERNARY GEOLOGY》 1997-01
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GEOLOGICAL CONFIGURATION AND EVOLUTION OF THE FAULT ZONE IN THE EAST OF THE XIHU DEPRESSION

Gong Jianming Chen Guowei (Institute of Marine Geology,MGMR,Qingdao,266071,China)  
On the basis of careful studies of seismic sections across the fault zone in the east of the Xihu depression,it is discovered that the fault zone,as the boundary of the Xihu depression,was not a whole before the end of Oligocene.Only after the first episode of Longjing motion did the fault zone become connected.At the middle part of Diaoyudao Uplift to the east of the fault zone,are Early Tertiary strata in which magmatic intrusion is found.Most of local structures in the fault zone were formed at the end of Oligocene(T 4 2).Among them,fault anticlines and reverse drag anticlines prevail.Because most structures were destroyed by magmatic intrusions and faults,it is very difficult for these structures to preserve oil and gas.
【CateGory Index】: P736.1
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