Sinistral strike slip of the Zhangjiakou-Penglai Fault and its control on hydrocarbon accumulation in the northeast of Shaleitian Bulge, Bohai Bay Basin, East China

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 anal...

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Main Authors: Jingsong PENG, Ajuan WEI, Zhe SUN, Xinlu CHEN, Dijiang ZHAO
Format: Article
Language:English
Published: KeAi Communications Co., Ltd. 2018-04-01
Series:Petroleum Exploration and Development
Online Access:http://www.sciencedirect.com/science/article/pii/S1876380418300259
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spelling doaj-76421b92710043a9a6d839520bfdab612021-02-02T00:54:02ZengKeAi Communications Co., Ltd.Petroleum Exploration and Development1876-38042018-04-01452215226Sinistral strike slip of the Zhangjiakou-Penglai Fault and its control on hydrocarbon accumulation in the northeast of Shaleitian Bulge, Bohai Bay Basin, East ChinaJingsong PENG0Ajuan WEI1Zhe SUN2Xinlu CHEN3Dijiang ZHAO4Corresponding author; CNOOC Tianjin Company, Tianjin 300452, ChinaCNOOC Tianjin Company, Tianjin 300452, ChinaCNOOC Tianjin Company, Tianjin 300452, ChinaCNOOC Tianjin Company, Tianjin 300452, ChinaCNOOC Tianjin Company, Tianjin 300452, ChinaThe 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. Key words: Bohai Bay Basin, Zhangjiakou-Penglai Fault, Tan-Lu Fault, sinistral strike slip, fault throw, hydrocarbon injectionhttp://www.sciencedirect.com/science/article/pii/S1876380418300259
collection DOAJ
language English
format Article
sources DOAJ
author Jingsong PENG
Ajuan WEI
Zhe SUN
Xinlu CHEN
Dijiang ZHAO
spellingShingle Jingsong PENG
Ajuan WEI
Zhe SUN
Xinlu CHEN
Dijiang ZHAO
Sinistral strike slip of the Zhangjiakou-Penglai Fault and its control on hydrocarbon accumulation in the northeast of Shaleitian Bulge, Bohai Bay Basin, East China
Petroleum Exploration and Development
author_facet Jingsong PENG
Ajuan WEI
Zhe SUN
Xinlu CHEN
Dijiang ZHAO
author_sort Jingsong PENG
title Sinistral strike slip of the Zhangjiakou-Penglai Fault and its control on hydrocarbon accumulation in the northeast of Shaleitian Bulge, Bohai Bay Basin, East China
title_short Sinistral strike slip of the Zhangjiakou-Penglai Fault and its control on hydrocarbon accumulation in the northeast of Shaleitian Bulge, Bohai Bay Basin, East China
title_full Sinistral strike slip of the Zhangjiakou-Penglai Fault and its control on hydrocarbon accumulation in the northeast of Shaleitian Bulge, Bohai Bay Basin, East China
title_fullStr Sinistral strike slip of the Zhangjiakou-Penglai Fault and its control on hydrocarbon accumulation in the northeast of Shaleitian Bulge, Bohai Bay Basin, East China
title_full_unstemmed Sinistral strike slip of the Zhangjiakou-Penglai Fault and its control on hydrocarbon accumulation in the northeast of Shaleitian Bulge, Bohai Bay Basin, East China
title_sort sinistral strike slip of the zhangjiakou-penglai fault and its control on hydrocarbon accumulation in the northeast of shaleitian bulge, bohai bay basin, east china
publisher KeAi Communications Co., Ltd.
series Petroleum Exploration and Development
issn 1876-3804
publishDate 2018-04-01
description 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. Key words: Bohai Bay Basin, Zhangjiakou-Penglai Fault, Tan-Lu Fault, sinistral strike slip, fault throw, hydrocarbon injection
url http://www.sciencedirect.com/science/article/pii/S1876380418300259
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