作者:张震;张新涛;徐春强;吴庆勋;李龙; 时间:2019-01-01 点击数:
张震;张新涛;徐春强;吴庆勋;李龙;
1:中海石油(中国)有限公司天津分公司
摘要(Abstract):
受多期构造运动影响,渤海海域428潜山的构造演化过程相对复杂。根据新三维地震和钻井资料,采用水平相干体技术,分析428潜山的地层结构和构造特征,探讨构造成因演化及其对油气成藏的影响。结果表明:研究区潜山东、西两个构造脊分别具有古生界和前寒武系、中生界和前寒武系双层结构特征;经历印支运动期的近SN向逆冲挤压、燕山运动早期的NW向继承性挤压、燕山运动中期的NW-SE向强烈伸展断陷、燕山运动晚期的NWW向挤压隆升,以及喜山运动期以来的伸展、走滑复合叠加改造,428潜山发育长期活动、早期活动和晚期活动3类断层,一系列网格状裂缝及多个不整合面改善潜山储层物性,增强油气输导能力。该结果为渤中坳陷区域内潜山油气勘探提供参考。
关键词(KeyWords):地层结构;构造演化;控藏作用;428潜山;渤海海域
Abstract:
Keywords:
基金项目(Foundation):国家科技重大专项(2016ZX05024-002-006)
作者(Author):张震;张新涛;徐春强;吴庆勋;李龙;
Email:
参考文献(References):
[1]薛永安,李慧勇.渤海海域深层太古界变质岩潜山大型凝析气田的发现及其地质意义[J].中国海上油气,2018,30(3):1-9.XUE Yongan,LI Huiyong.Large condensate gas field in deep Archean metamorphic buried hill in Bohai Sea:discovery and geological significance[J].China Offshore Oil and Gas,2018,30(3):1-9.
[2]郭颖,王粤川,韦阿娟,等.潜山内幕火山岩储层特征及控制因素:以渤海海域秦皇岛30A地区白垩系为例[J].沉积学报,2017,35(2):343-355.GUO Ying,WANG Yuechuan,WEI Ajuan,et al.Characteristics and controlling factors of buried-hill inner volcanic reservoir:an example from the Cretaceous in Qinhuangdao 30A Area,offshore Bohai Sea,China[J].Acta Sedimentologica Sinica,2017,35(2):343-355.
[3]胡贺伟,李慧勇,于海波,等.渤中21-22构造区断层演化及其对油气的控制作用[J].东北石油大学学报,2016,40(2):36-46.HU Hewei,LI Huiyong,YU Haibo,et al.Fracture evolution of Bozhong 21-22structure area and their control on hydrocarbons[J].Journal of Northeast Petroleum University,2016,40(2):36-46.
[4]邓运华.渤海大中型潜山油气田形成机理与勘探实践[J].石油学报,2015,36(3):253-261.DENG Yunhua.Formation mechanism and exploration practice of large-medium buried-hill oil fields in Bohai Sea[J].Acta Petrolei Sinica,2015,36(3):253-261.
[5]王纯,张研,吴小洲,等.辽河滩海地区东部构造演化与潜山带内幕油气聚集[J].东北石油大学学报,2017,41(1):43-51.WANG Chun,ZHANG Yan,WU Xiaozhou,et al.Tectonic evolution of eastern Liaohe offshore and hydrocarbon accumulation of interior buried hill[J].Journal of Northeast Petroleum University,2017,41(1):43-51.
[6]周心怀,张如才,李慧勇,等.渤海湾盆地渤中凹陷深埋古潜山天然气成藏主控因素探讨[J].中国石油大学学报(自然科学版),2017,41(1):43-49.ZHOU Xinhuai,ZHANG Rucai,LI Huiyong,et al.Major controls on natural gas accumulations in deep-buried hills in Bozhong Depression,Bohai Bay Basin[J].Journal of China University of Petroleum(Edition of Natural Science),2017,41(1):43-49.
[7]高长海,查明,赵贤正,等.渤海湾盆地冀中坳陷深层古潜山油气成藏模式及其主控因素[J].天然气工业,2017,37(4):52-58.GAO Changhai,ZHA Ming,ZHAO Xianzheng,et al.Hydrocarbon accumulation models and their main controlling factors in the deep buried hills of the Jizhong Depression,Bohai Bay Basin[J].Natural Gas Industry,2017,37(4):52-58.
[8]赵凯,蒋有录,刘华,等.济阳坳陷孤岛与埕岛潜山油气差异富集原因分析[J].地质力学学报,2018,24(2):220-226.ZHAO Kai,JIANG Youlu,LIU Hua,et al.Analysis on the causes of different enrichment of hydrocarbon in Gudao and Chengdao Buried-hills,Jiyang Depression[J].Journal of Geomechanics,2018,24(2):220-226.
[9]李岳桐,王文庆,卢刚臣,等.黄骅坳陷潜山成因分类及其意义[J].东北石油大学学报,2018,42(3):75-83.LI Yuetong,WANG Wenqing,LU Gangchen,et al.Genetic classification of buried hills and its significance of Huanghua Depression[J].Journal of Northeast Petroleum University,2018,42(3):75-83.
[10]付立新,楼达,李宏军,等.印支-燕山运动对大港探区古潜山形成的控制作用[J].石油学报,2016,37(增刊2):19-30.FU Lixin,LOU Da,LI Hongjun,et al.Control effect of Indosinian-Yanshan movement on the formation of buried hill in Dagang Exploration Area[J].Acta Petrolei Sinica,2016,37(Supp.2):19-30.
[11]周心怀,胡志伟,韦阿娟,等.渤海海域蓬莱9-1大型复合油田潜山发育演化及其控藏作用[J].大地构造与成矿学,2015,39(4):680-690.ZHOU Xinhuai,HU Zhiwei,WEI Ajuan,et al.Tectonic origin and evolution and their controls on accumulation of Penglai 9-1Large Composite Oilfield buried hill in Bohai Sea[J].Geotectonica et Metallogenia,2015,39(4):680-690.
[12]何登发,崔永谦,张煜颖,等.渤海湾盆地冀中坳陷古潜山的构造成因类型[J].岩石学报,2017,33(4):1338-1356.HE Dengfa,CUI Yongqian,ZHANG Yuying,et al.Structural genetic types of paleoburied hill in Jizhong Depression,Bohai Bay Basin[J].Acta Petrologica Sinica,2017,33(4):1338-1356.
[13]杨海风,魏刚,王德英,等.秦南凹陷秦皇岛29-2油气田原油来源及其勘探意义[J].油气地质与采收率,2011,18(6):28-31.YANG Haifeng,WEI Gang,WANG Deying,et al.Oil sources and exploration significance of Qinhuangdao29-2Oil-Gas Field[J].Petroleum Geology and Recovery Efficiency,2011,18(6):28-31.
[14]李三忠,索艳慧,戴黎明,等.渤海湾盆地形成与华北克拉通破坏[J].地学前缘,2010,17(4)64-89.LI Sanzhong,SUO Yanhui,DAI Liming,et al.Development of the Bohai Bay Basin and destruction of the North China Craton[J].Earth Science Frontiers,2010,17(4)64-89.
[15]朱伟林,米立军,龚再升,等.渤海海域油气成藏与勘探[M].北京:科学出版社,2009:1-3.ZHU Weilin,MI Lijun,GONG Zaisheng,et al.Bohai Sea oil and gas exploration[M].Beijing:Science Press,2009:1-3.
[16]纪友亮,胡光明,吴志平,等.渤海湾中生代地层剥蚀量及盆地演化[J].天然气工业,2004,24(12):28-31.JI Youliang,HU Guangming,WU Zhiping,et al.Eroded thickness of Mesozoic in Bohai Gulf and basin evolution[J].Natural Gas Industry,2004,24(12):28-31.
[17]夏庆龙,田立新,周心怀,等.渤海海域构造形成演化与变化机制[M].北京:石油工业出版社,2012:60-63,106.XIA Qinglong,TIAN Lixin,ZHOU Xinhuai,et al.structure evaluation and deformation mechanism in Bohai Sea Area[M].Beijing:Petroleum Industry Press,2012:60-63,106.
[18]马龙,刘全新,张景廉,等.论基岩油气藏的勘探前景[J].天然气工业,2006,26(1):8-11.MA Long,LIU Quanxin,ZHANG Jinglian,et al.A discussion of exploration potentials of basement hydrocarbon reservoir[J].Natural Gas Industry,2006,26(1):8-11.
[19]郝芳,蔡东升,邹华耀,等.渤中坳陷超压-构造活动联控型流体流动与油气快速成藏[J].地球科学,2004,29(5):518-524.HAO Fang,CAI Dongsheng,ZOU Huayao,et al.Overpressure-tectonic activity controlled fluid flow and rapid petroleum accumulation in Bozhong Depression,Bohai Bay Basin[J].Earth Science,2004,29(5):518-524.
[20]刘晓峰,解习农,张成,等.渤海湾盆地渤中坳陷储层超压特征与成因机制[J].地球科学,2008,33(3):337-341.LIU Xiaofeng,XIE Xinong,ZHANG Cheng,et al.Characteristics and generation of the reservoir overpressure in Bozhong Depression,Bohai Bay Basin[J].Earth Science,2008,33(3):337-341.
[21]蒋有录,王鑫,于倩倩,等.渤海湾盆地含油气凹陷压力场特征及与油气富集关系[J].石油学报,2016,37(11):1362-1368.JIANG Youlu,WANG Xin,YU Qianqian,et al.Pressure field characteristics of petroliferous depressions and its relationship with hydrocarbon enrichment in Bohai Bay Basin[J].Acta Petrolei Sinica,2016,37(11):1362-1368.
[22]赵莉莉.环渤中地区地层压力特征及其与油气分布的关系[D].成都:成都理工大学,2013:65-67.ZHAO Lili.Characteristics of formation pressure and its relationship with the oil and gas distribution in the Bozhong Area[D].Chengdu:Chengdu University of Technology,2013:65-67.
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