张家口——蓬莱断裂渤海沙垒田凸起东北段盆岭再造及其对油气成藏的影响
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摘要
以三维地震和钻井资料为基础,通过地震属性分析、构造几何学分析、断层活动性分析、构造演化史分析和油气运移模拟等方法,对张家口—蓬莱断裂带渤海沙垒田凸起东北段的构造样式、断裂活动性、走滑位移量、中央构造带的形成机制及其油气运聚进行分析。研究区是早期(古新世—始新世)伸展和晚期(渐新世、上新世—第四纪)走滑-拉分的叠合构造区;张家口—蓬莱断裂渤海沙垒田凸起东北段左旋走滑活动有两个阶段,即渐新世和上新世—第四纪,渤海海域活动较陆地段更早;新生代以来左旋走滑位移量共4 km,其中渐新世活动较弱(1 km),上新世较强(3 km);大规模的走滑活动导致了断裂带围区断裂活动的加剧和盆岭再造,促进了中央构造带的形成和北东向构造带的协同演化;张家口—蓬莱断裂渤海沙垒田凸起东北段及其共轭走滑断裂带剧烈的新构造运动控制了油气从深层往浅层运移的充注点/段,从而控制了其浅层油气运移及成藏。图13表1参48
The structural style, fault activity, strike-slip displacement, and the formation mechanism and hydrocarbon migration and accumulation in the center tectonic zone in the northeast Shaleitian Bulge of Zhangjiakou-Penglai Fault Zone were studied by seismic attribute analysis, structural geometric analysis, fault activity analysis, structure evolution history and simulation of hydrocarbon migration, based on 3-D seismic and drilling data. The main results are as follows:(1) The study area is a superimposed tectonic zone, which experienced early(Paleocene and Eocene) extension and late(Oligocene and Pliocene-Quaternary) strike-slip and pull-apart.(2) The sinistral strike slip of the northeast Shaleitian Bulge of Zhangjiakou-Penglai Fault Zone went through two periods, Oligocene and Pliocene-Quaternary, and the Bohai section was active earlier than the inland section.(3) The sinistral strike slip displacement of Zhangjiakou-Penglai Fault is 4 km since Cenozoic, including 1 km in the Oligocene, and 3 km in the Pliocene-Quaternary.(4) The strike-slip movements have resulted in the increase of fault activity and basin-mountain restructure in the fault zone, also contributed to the formation of the central tectonic belt and the conjugate evolution in north-east structural belt.(5) The conjugate strike slip of the Zhangjiakou-Penglai Fault Zone dominated the migration and accumulation of hydrocarbon in shallow formations by controlling the injection points and segments of hydrocarbon from the deep layers to shallow layers.
The structural style, fault activity, strike-slip displacement, and the formation mechanism and hydrocarbon migration and accumulation in the center tectonic zone in the northeast Shaleitian Bulge of Zhangjiakou-Penglai Fault Zone were studied by seismic attribute analysis, structural geometric analysis, fault activity analysis, structure evolution history and simulation of hydrocarbon migration, based on 3-D seismic and drilling data. The main results are as follows:(1) The study area is a superimposed tectonic zone, which experienced early(Paleocene and Eocene) extension and late(Oligocene and Pliocene-Quaternary) strike-slip and pull-apart.(2) The sinistral strike slip of the northeast Shaleitian Bulge of Zhangjiakou-Penglai Fault Zone went through two periods, Oligocene and Pliocene-Quaternary, and the Bohai section was active earlier than the inland section.(3) The sinistral strike slip displacement of Zhangjiakou-Penglai Fault is 4 km since Cenozoic, including 1 km in the Oligocene, and 3 km in the Pliocene-Quaternary.(4) The strike-slip movements have resulted in the increase of fault activity and basin-mountain restructure in the fault zone, also contributed to the formation of the central tectonic belt and the conjugate evolution in north-east structural belt.(5) The conjugate strike slip of the Zhangjiakou-Penglai Fault Zone dominated the migration and accumulation of hydrocarbon in shallow formations by controlling the injection points and segments of hydrocarbon from the deep layers to shallow layers.
引文
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