郯庐断裂带渤南段构造特征及其控盆作用
详细信息    查看全文 | 推荐本文 |
  • 英文篇名:Structural Characteristics of Tan-Lu Fault Zone in South Area of Bohai Sea and Its Control on Basin Structure
  • 作者:张婧 ; 李伟 ; 吴智平 ; 李春锐 ; 杨波 ; 张晓庆
  • 英文作者:Zhang Jing;Li Wei;Wu Zhiping;Li Chunrui;Yang Bo;Zhang Xiaoqing;School of Geosciences,China University of Petroleum;Laboratory for Marine Mineral Resources,Qingdao National Laboratory for Marine Science and Technology;Research Institute of Bohai Oil Field,CNOOC Tianjin Branch Company;
  • 关键词:构造特征 ; 构造演化 ; 走滑运动 ; 新生代 ; 郯庐断裂带 ; 渤南地区 ; 油气
  • 英文关键词:structural characteristics;;structural evolution;;strike-slip movement;;Cenozoic;;Tan-Lu fault zone;;south area of Bohai Sea;;hydrocarbons
  • 中文刊名:DQKX
  • 英文刊名:Earth Science
  • 机构:中国石油大学地球科学与技术学院;青岛海洋科学与技术国家实验室海洋矿产资源评价与探测技术功能实验室;中海石油有限公司天津分公司渤海油田勘探开发研究院;
  • 出版日期:2017-09-15
  • 出版单位:地球科学
  • 年:2017
  • 期:v.42
  • 基金:国家油气重大专项课题(No.2011ZX05023-006-05)
  • 语种:中文;
  • 页:DQKX201709009
  • 页数:16
  • CN:09
  • ISSN:42-1874/P
  • 分类号:112-127
摘要
渤南地区郯庐断裂带具有很好的油气勘探前景,但由于其构造特征复杂,目前对渤南地区油气成藏条件、主控因素及富集规律的认识尚不明晰.通过对三维地震和地质资料的分析解释,结合前人研究成果,探讨了渤南地区郯庐断裂带构造特征的时空差异及其对盆地结构的控制作用.研究表明,渤南地区郯庐断裂带具有3组分支断裂,每组分支断裂由2~4条断裂构成,均表现出了明显的走滑特征,整体由东向西、由深至浅走滑程度逐渐减弱.新生代古新世-早始新世郯庐断裂带渤南段左旋走滑,东部分带活动明显、强度大,中带和西带不活动或活动较弱,渤南地区中生代发育的NWW向伸展断裂系统复活,形成北断南超的复式半地堑或南北双断式结构;中始新世以来,渤南地区郯庐断裂带转为右旋走滑,3组分支断裂均开始活动,表现为强烈的走滑兼伸展运动,强度由东向西逐渐减弱,中带分支断裂形成的中央构造脊将黄河口凹陷分割成东、西两个次洼,并开始逐渐发育一系列次级断层,与主断裂构成帚状断裂组合;新近纪-第四纪郯庐断裂渤南段表现为右旋走滑兼挤压,主走滑断裂不连续,代之以大量规模较小的次级断裂系统.太平洋区板块俯冲方向、俯冲速率的变化以及深部动力背景的变迁共同造成了渤南地区郯庐断裂不同分支构造发育演化及其控盆作用的差异性,由于右旋走滑位移量小于先期的左旋走滑,现今渤南地区构造单元分布仍具左旋特征.
        Tan-Lu fault zone in the south area of Bohai Sea has a good prospect for oil and gas exploration.However,due to its complicated structural features,the understanding of hydrocarbon accumulation conditions,main controlling factors and enrichment regularity is not clear at present.On the basis of the previous studies,3D seismic data and geological information,the structural characteristics and spatiotemporal differences of Tan-Lu fault zone in the south area of Bohai Sea and the control of the development and evolution of Tan-Lu fault zone on the basin structure are studied in this paper.The results show that Tan-Lu fault zone in the south area of Bohai Sea has three branches,each of which is composed of 2-4 faults presenting strike-slip characteristics.The strike-slip strength gradually weakens westward.From Paleogene to Early Eocene,Tan-Lu fault zone in the south area of Bohai Sea presented sinistral strike-slip characteristics.The eastern branch experienced intense strike-slip movement,whereas the middle and western branches moved slightly,and the NWW-trending extensional faults which developed in Mesozoic renewed.Basin in the south area of Bohai Sea shows as a halfgraben with northern-faulted and southern-overlapped structural setting or a graben with both northern and southern faulted settings.From the Middle Eocene,Tan-Lu fault zone turned into dextral strike-slip movement.The three branches started to activate and showed both strike-slip and extensional properties.The intensity of fault activity gradually weakened from east to west.The middle branch divided the Huanghekou sag into two subsags.A series of secondary faults formed the broom-like structure combined with the main fault.From Neogene to Quaternary,Tan-Lu fault zone presented dextral strike-slip as well as extrusion movement in the study area and a large number of small-scale secondary faults have developed.The change of subduction direction and rate of Pacific plate and the variation of deep geodynamics mechanism induce the differences of the evolution process of three branches and their controlling effect on the basin structure.Since the strength of dextral strike-slip movement is less than that of sinistral strike-slip,the distribution of the structural units in the south area of Bohai Sea are still showing the sinistral strike-slip characteristic now.
引文
Cai,D.S.,Luo,Y.H.,Wu,W.L.,et al.,2001.Shallow Tectonic Deformation and Its Relationship to Hydrocarbon Enrichment in Bozhong Depression and Adjacent Areas,Bohai Bay Basin.China Offshore Oil and Gas(Geology),15(1):35-43(in Chinese with English abstract).
    Chen,J.,2004.Characteristics and Prospecting Meaning of Sedimentary Basin in Structural Transitional Stages in Kongdian Formation of Jiyang Depression.Progress in Geophysics,19(2):392-398(in Chinese with English abstract).
    Chen,S.P.,Lü,D.Y.,Wang,Y.B.,et al.,2010.NeogeneQuaternary Strike-Slip Movement in Bohai Basin and Its Significance in Petroleum Exploration.Acta Petrolei Sinica,31(6):894-899(in Chinese with English abstract).
    Deng,Y.H.,2004.Tensional-Shear Faults and Analysis of Oil and Gas Migration-Taking Bohai Oil Province for Example.China Petroleum Exploration,9(2):33-37(in Chinese with English abstract).
    Ding,Z.Y.,Wang,L.S.,Zhong,K.,et al.,2008.Distribution Characteristics and Tectonic Significance of Cenozoic Remnant Formation,Bohai Bay Basin.Geological Journal of China Universities,14(3):405-413(in Chinese with English abstract).
    Engebretson,D.C.,Cox,A.,Gordon,R.G.,1985.Relative Motions between Oceanic and Continental Plates in the Pacific Basin.Geological Society of America Special Papers,93:1-60.doi:10.1130/spe206-p1
    Fu,Q.,Liu,B.B.,Xu,C.H.,et al.2013.The Couple Relationship of Quantitative Analysis of the Structures and Oil&Gas Accumulation in Huanghekou Depression,Bohai Bay Basin.Acta Petrolei Sinica,34(Suppl.2):112-119(in Chinese with English abstract).
    Gilder,S.A.,Leloup,P.H.,Courtillot,V.,et al.,1999.Tectonic Evolution of the Tancheng-Lujiang(Tan-Lu)Fault via Middle Triassic to Early Cenozoic Paleomagnetic Data.Journal of Geophysical Research:Solid Earth,104(B7):15365-15390.doi:10.1029/1999JB900123
    Grimmer,J.C.,Jonckheere,R.,Enkelmann,E.,et al.,2002.Cretaceous-Cenozoic History of the Southern Tan-Lu Fault Zone:Apatite Fission-Track and Structural Constraints from the Dabie Shan(Eastern China).Tectonophysics,359(3-4):225-253.doi:10.1016/s0040-1951(02)00513-9
    Hou,G.T.,2014.Geodynamics of Bohai Basin.Science Press,Beijing(in Chinese).
    Hou,G.T.,Qian,X.L.,Cai,D.S.,2000.Space-Time Relationship between Tectonics and Sedimentation of MesoCenozoic Bohai Basin.Oil&Gas Geology,21(3):201-206(in Chinese with English abstract).
    Hou,G.T.,Qian,X.L.,Cai,D.S.,2001.The Tectonic Evolution of Bohai Basin in Mesozoic and Cenozoic Time.Acta Scientiarum Naturalium Universitatis Pekinensis,37(6):845-851(in Chinese with English abstract).
    Hou,G.,Hari,K.R.,2014.Mesozoic-Cenozoic Extension of the Bohai Sea:Contribution to the Destruction of North China Craton.Frontiers of Earth Science,8(2):202-215.doi:10.1007/s11707-014-0413-3
    Hou,M.J.,Zhu,G.,Mercier,J.,et al.,2007.Analyzing on Geodynamics and Regional Tectonic Evolution of the TanLu Fault Zone(Anhui Segment)and Its Environs.Chinese Journal of Geology:Scientia Geologica Sinica,42(2):362-381(in Chinese with English abstract).
    Hu,W.,Zhu,G.,Yan,L.J.,et al.,2014.Analysis of Relationship between Seismic Activity and Crust Electrical Textures for the Central Segment of the Tan-Lu Fault Zone.Geological Review,60(1):80-90(in Chinese with English abstract).
    Hu,X.G.,Tan,M.Y.,Zhang,M.Z.,2007.The Strike-Slip Structure in the East of Jiyang Depression.Petroleum Geophysics,(1):50-54,58(in Chinese with English abstract).
    Huang,C.,Yu,C.H.,Zhang,G.L.,et al.,2013.Cenozoic Dextral Strike-Slip Displacement of the Middle Tan-Lu Fault Zone.Journal of Jilin University:Earth Science Edition,43(3):820-832(in Chinese with English abstract).
    Huang,L.,Wang,Y.B.,Wu,Q.,et al.,2012.Cenozoic Tectonic Evolution of the Laizhouwan Sag in Bohai Bay Basin.Acta Geologica Sinica,86(6):867-876(in Chinese with English abstract).
    Jiang,J.P.,2008.Cenozoic Kinematics of the Yingkou-Weifang Fault Zone in Eastern China.Marine Geology&Quaternary Geology,28(4):57-64(in Chinese with English abstract).
    Kopp,H.,Flueh,E.R.,Klaeschen,D.,et al.,2001.Crustal Structure of the Central Sunda Margin at the Onset of Oblique Subduction.Geophysical Journal International,147(2):449-474.doi:10.1046/j.0956-540x.2001.01547.x
    Kopp,H.,Kopp,C.,Phipps Morgan,J.,et al.,2003.Fossil Hot Spot-Ridge Interaction in the Musicians Seamount Province:Geophysical Investigations of Hot Spot Volcanism at Volcanic Elongated Ridges.Journal of Geophysical Research:Solid Earth,108(B3):2160.doi:10.1029/2002jb002015
    Li,S.Z.,Suo,Y.H.,Dai,L.M.,et al.,2010.Development of the Bohai Bay Basin and Destruction of the North China Craton.Earth Science Frontiers,17(4):64-89(in Chinese with English abstract).
    Li,W.,2007.Mesozoic Basin Evolution and the Exploration of the Pre-Tertiary Petroleum in the Area of Bohai Bay Basin(Dissertation).China University of Petroleum,Dongying(in Chinese with English abstract).
    Li,W.,Wu,Z.P.,Liu,H.,2009.Mesozoic and Cenozoic Basin Evolution and Coal-Derived Gas Accumulation of Upper Paleozoic in the Area of Bohai Bay Basin.Petroleum Geology and Recovery Efficiency,16(1):13-16(in Chinese with English abstract).
    Li,W.,Wu,Z.P.,Zhao,W.D.,2010.Structural Characteristics and Basin Transformation in the Bohai Bay Basin in the Yanshan Era.Progress in Geophysics,25(6):2068-2077(in Chinese with English abstract).
    Li,W.,Wu,Z.P.,Zhou,Y.Q.,2005.Reconstruction of the Thickness of the Mesozoic Strata and Mesozoic Prototype Basin in the Jiyang Depression.Geological Review,51(5):507-516(in Chinese with English abstract).
    Lü,D.Y.,Hou,D.M.,Yang,Q.H.,et al.,2011.A Study on Structure Origins and Hydrocarbon Accumulation Pattern in the West Part of Bonan Lower-Uplift.China Offshore Oil and Gas,23(4):229-233(in Chinese with English abstract).
    Meng,Q.R.,Li,S.Y.,Li,R.W.,2007.Mesozoic Evolution of the Hefei Basin in Eastern China:Sedimentary Response to Deformations in the Adjacent Dabieshan and along the Tanlu Fault.Geological Society of America Bulletin,119(7-8):897-916.doi:10.1130/b25931.1
    Niu,C.M.,2012.Tectonic Evolution and Hydrocarbon Accumulation of Laizhouwan Depression in Southern Bohai Sea.Oil&Gas Geology,33(3):424-431(in Chinese with English abstract).
    Northrup,C.J.,Royden,L.H.,Burchfiel,B.C.,1995.Motion of the Pacific Plate Relative to Eurasia and Its Potential Relation to Cenozoic Extension along the Eastern Margin of Eurasia.Geology,23(8):719.doi:10.1130/0091-7613(1995)023<0719:motppr>2.3.co;2
    Peng,W.X.,Shi,H.,Sun,H.F.,et al.,2009a.Dextral StrikeSlip Evidence on Seismic Slice for Tanlu Strike-Slip Fault.Oil Geophysical Prospecting,44(6):755-759,783,649(in Chinese with English abstract).
    Peng,W.X.,Xin,R.C.,Sun,H.F.,et al.,2009b.Formation and Evolution of Laizhou Bay Sag in Bohai Bay.Acta Petrolei Sinica,30(5):654-660(in Chinese with English abstract).
    Peng,W.X.,Zhang,R.C.,Sun,H.F.,et al.,2010.Displacement of the Tanlu Fault since Paleocene and Its Influence on the Laizhou Bay Sag,Bohai Bay Basin of China.Geotectonica et Metallogenia,34(4):585-592(in Chinese with English abstract).
    Qi,J.F.,2004.Two Tectonic Systems in the Cenozoic Bohai Bay Basin and their Genetic Interpretation.Chinese Geology,31(1):15-22(in Chinese with English abstract).
    Qi,J.F.,Zhou,X.H.,Wang,Q.S.,2010.Structural Model and Cenozoic Kinematics of Tan-Lu Deep Fracture Zone in Bohai Sea Area.Geology in China,37(5):1231-1242(in Chinese with English abstract).
    Qi,J.F.,Deng,R.J.,Zhou,X.H.,et al.,2008.Structural Characteristics of the Tan-Lu Fault Zone in Cenozoic Basins Offshore the Bohai Sea.Science in China(Ser.D),38(Suppl.1):19-29(in Chinese).
    Ren,J.Y.,2004.Tectonic Significance of S_(6')Boundary in Dongying Depression,Bohai Gulf Basin.Earth Science,29(1):69-76,92(in Chinese with English abstract).
    Shan,J.Z.,Zhang,Z.W.,Sun,H.J.,et al.,2004.Modeling Experiments of Generation Mechanism of YingkouTongerbu Fracture Zone in the Liaohe Depression.Petroleum Exploration and Development,31(1):15-17(in Chinese with English abstract).
    Song,G.Q.,2006.Magnetotelluric Depth Sounding Sections of Tan-Lu Fault Zone and Its Crustal Structure in Shandong,Jiangsu and Anhui Provinces.Petroleum Geology and Recovery Efficiency,13(6):1-4(in Chinese with English abstract).
    Steinberger,B.,Sutherland,R.,O'Connell,R.J.,2004.Prediction of Emperor-Hawaii Seamount Locations from a Revised Model of Global Plate Motion and Mantle Flow.Nature,430(6996):167-173.doi:10.1038/nature02660
    Sun,H.F.,Zhou,X.H.,Peng,W.X.,et al.,2011.Late-Stage Hydrocarbon Accumulation and Enrichment in the Huanghekou Sag,Southern Bahai Sea.Petroleum Exploration and Development,38(3):307-313(in Chinese with English abstract).
    Sun,X.M.,Wang,S.Q.,Wang,Y.D.,et al.,2010.The Structural Feature and Evolutionary Series in the Northern Segment of Tancheng-Lujiang Fault Zone.Acta Petrologica Sinica,26(1):165-176(in Chinese with English abstract).
    Suo,Y.H.,Li,S.Z.,Xu,L.Q.,et al.,2015.Cenozoic Structural Evolution and Prototype Basin of the Great Qikou Sag,the Bohai Bay Basin.Chinese Journal of Geology,50(2):473-488(in Chinese with English abstract).
    Tang,L.J.,Chen,X.Y.,Zhou,X.H.,et al.,2011.Structural Analysis of Tan-Lu Fault Zone in the Bohai Sea.Journal of Southwest Petroleum University(Seience&Technology Edition),33(1):170-176(in Chinese with English abstract).
    Tong,H.M.,Mi,R.S.,Yu,T.C.,et al.,2008.The Strike-Slip Tectonics in the Western Liaohe Depression,Bohai Bay Basin.Acta Geologica Sinica,82(8):1017-1026(in Chinese with English abstract).
    Wan,G.M.,Tang,L.J.,Zhou,X.H.,et al.,2010.NeogeneQuaternary Fault Characteristics and Its Formation Mechanism in Bohai Sea.Acta Petrolei Sinica,31(4):591-595(in Chinese with English abstract).
    Wan,T.F.,Zhu,H.,2002.Tectonics and Environment Change of Meso-Cenozoicin China Continent and Its Adjacent Areas.Geoscience,16(2):107-120(in Chinese with English abstract).
    Wang,G.C.,1998.Relationship of Tanlu Fault to the Inversion and Flower Structures in Bohai Bay.China Offshore Oil And Gas(Geology),(5):1-7(in Chinese with English abstract).
    Wu,F.Y.,Xu,Y.G.,Gao,S.,et al.,2008.Lithospheric Thinning and Destruction of the North China Craton.Acta Petrologica Sinica,24(6):1145-1174(in Chinese with English abstract).
    Wu,G.Q.,Lü,X.X.,Zhou,X.H.,et al.,2013.Response of Cenozoic Tan-Lu Fault Activity in Laizhou Bay Area,Bohai Sea.Petroleum Geology and Experiment,35(4):407-413(in Chinese with English abstract).
    Wu,Z.P.,Hou,X.B.,Li,W.,2007.Discussion on Mesozoic Basin Patterns and Evolution in the Eastern North China Block.Geotectonica et Metallogenia,31(4):385-399(in Chinese with English abstract).
    Xu,C.G.,2016.Strike-Slip Transfer Zone and Its Control on Formation of Medium and Large-Sized Oilfields in Bohai Sea Area.Earth Science,41(9):1548-1560(in Chinese with English abstract).
    Xu,L.Q.,Li,S.Z.,Suo,Y.H.,et al.,2015.Fault System and Basin Prototype of the Great Qikou Sag,Bohai Bay Basin.Chinese Journal of Geology,50(2):489-502(in Chinese with English abstract).
    Xu,Y.D.,Liu,Z.Q.,2006.Strike-Slip Tectonic Characteristics of Yingwei Fault Zone.Journal of Oil and Gas Technology,28(6):12-15(in Chinese with English abstract).
    Yan,L.J.,2013.Neotectonic Active Characteristics and Dynamic Mechanism of the Shandong Segment of the TanLu Fault Zone(Dissertation).Hefei University of Technology,Hefei(in Chinese with English abstract).
    Zhang,M.Z.,Fu,J.P.,Yin,X.Y.,2006.Characters of StrikeSlip and Extrusion Structure in Zhuanghai Region.Petroleum Geology and Recovery Efficiency,13(2):5-7(in Chinese with English abstract).
    Zhang,M.Z.,Fu,J.P.,Yin,X.Y.,2006.Characters of StrikeSlip and Extrusion Structure in Zhuanghai Region.Petroleum Geology and Recovery Efficiency,13(2):5-7(in Chinese with English abstract).
    Zhang,P.,Wang,L.S.,Shi,H.S.,et al.,2010.The MesozoicCenozoic Tectonic Evolution of the Shandong Segment of the Tan-Lu Fault Zone.Acta Geologica Sinica,84(9):1316-1323(in Chinese with English abstract).
    Zhang,X.T.,Zhou,X.H.,Niu,C.M.,et al.,2014.Hydrocarbon Accumulation Mode in Huanghekou Sag of Bohai Basin.Journal of Oil and Gas Technology,36(3):30-36(in Chinese with English abstract).
    Zhang,Y.Q.,Dong,S.W.,2008.Mesozoic Tectonic Evolution History of the Tan-Lu Fault Zone,China:Advances and New Understanding.Geological Bulletin of China,27(9):1371-1390(in Chinese with English abstract).
    Zhou,B.,Deng,Z.H.,Chao,H.T.,et al.,2008.Strike-Slip Tectonic Characteristics,Evolution and Dynamic Mechanism of Yingwei Fault Zone.Northwestern Seismological Journal,30(2):117-123(in Chinese with English abstract).
    Zhou,W.W.,Wang,W.F.,An,B.,et al.,2014.Identification of Potential Fault Zones and Its Geological Significance in Bohai Bay Basin.Earth Science,39(11):1627-1638(in Chinese with English abstract).
    Zhu,G.,Niu,M.L.,Xie,C.L.,et al.,2010.Sinistral to Normal Faulting along the Tan-Lu Fault Zone:Evidence for Geodynamic Switching of the East China Continental Margin.The Journal of Geology,118(3):277-293.doi:10.1086/651540
    Zhu,G.,Wang,D.X.,Liu,G.S.,et al.,2001.Extensional Activities along the Tan-Lu Fault Zone and Its Geodynamic Setting.Chinese Journal of Geology,36(3):269-278(in Chinese with English abstract).
    Zhu,G.,Wang,Y.S.,Niu,M.L.,et al.,2004.Synorogenic Movement of the Tan-Lu Fault Zone.Earth Science Frontiers,11(3):169-182(in Chinese with English abstract).
    Zhu,G.,Wang,Y.S.,Liu,G.S.,et al.,2005.40 Ar/39 Ar Dating of Strike-Slip Motion on the Tan-Lu Fault Zone,East China.Journal of Structural Geology,27(8):1379-1398.doi:10.1016/j.jsg.2005.04.007
    Zhu,G.,Xu,Y.D.,Liu,G.S.,et al.,2006.Structural and Deformational Characteristics of Strike-Slippings along the Middle-Southern Sector of the Tan-Lu Fault Zone.Chinese Journal of Geology,41(2):226-241,255(in Chinese with English abstract).
    Zhu,X.X.,Lü,X.X.,Wang,D.Y.,et al.,2009.Controlling Effect of a Strike-Slip Transform Belt on Hydrocarbon Accumulations in the Huanghekou Sag,the Bohai Sea Waters.Oil&Gas Geology,30(4):476-482(in Chinese with English abstract).
    蔡东升,罗毓晖,武文来,等,2001.渤海浅层构造变形特征、成因机理与渤中坳陷及其周围油气富集的关系.中国海上油气(地质),15(1):35-43.
    陈洁,2004.济阳孔店构造转型期沉积盆地的特征及勘探意义.地球物理学进展,19(2):392-398.
    陈书平,吕丁友,王应斌,等,2010.渤海盆地新近纪-第四纪走滑作用及油气勘探意义.石油学报,31(6):894-899.
    邓运华,2004.张-扭断裂与油气运移分析---以渤海油区为例.中国石油勘探,9(2):33-37.
    丁增勇,王良书,钟锴,等,2008.渤海湾盆地新生界残留地层分布特征及其构造意义.高校地质学报,14(3):405-413.
    傅强,刘彬彬,徐春华,等,2013.渤海湾盆地黄河口凹陷构造定量分析与油气富集耦合关系.石油学报,34(z2):112-119.
    侯贵廷,2014.渤海湾盆地地球动力学.北京:科学出版社.
    侯贵廷,钱祥麟,蔡东升,2000.渤海中、新生代盆地构造活动与沉积作用的时空关系.石油与天然气地质,21(3):201-206.
    侯贵廷,钱祥麟,蔡东升,2001.渤海湾盆地中、新生代构造演化研究.北京大学学报:自然科学版,37(6):845-851.
    侯明金,朱光,Mercier,J.,等,2007.郯庐断裂带(安徽段)及邻区的动力学分析与区域构造演化.地质科学,42(2):362-381.
    胡惟,朱光,严乐佳,等,2014.郯庐断裂带中段地震活动性与深部地壳电性结构关系的探讨.地质论评,60(1):80-90.
    胡贤根,谭明友,张明振,2007.济阳坳陷东部走滑构造形成机制.油气地球物理,(1):50-54,58.
    黄超,余朝华,张桂林,等,2013.郯庐断裂中段新生代右行走滑位移.吉林大学学报:地球科学版,43(3):820-832.
    黄雷,王应斌,武强,等,2012.渤海湾盆地莱州湾凹陷新生代盆地演化.地质学报,86(6):867-876.
    姜建平,2008.营口-潍坊断裂带新生代运动学特征.海洋地质与第四纪地质,28(4):57-64.
    李三忠,索艳慧,戴黎明,等,2010.渤海湾盆地形成与华北克拉通破坏.地学前缘,17(4):64-89.
    李伟,2007.渤海湾盆地区中生代盆地演化与前第三系油气勘探(博士学位论文).东营:中国石油大学.
    李伟,吴智平,刘华,2009.中、新生代渤海湾盆地区演化与上古生界煤成气成藏.油气地质与采收率,16(1):13-16.
    李伟,吴智平,赵文栋,2010.渤海湾盆地区燕山期构造特征与盆地转型.地球物理学进展,25(6):2068-2077.
    李伟,吴智平,周瑶琪,2005.济阳坳陷中生代地层剥蚀厚度、原始厚度恢复及原型盆地研究.地质论评,51(5):507-516.
    吕丁友,侯东梅,杨庆红,等,2011.渤南低凸起西段构造成因机制与油气成藏规律研究.中国海上油气,23(4):229-233.
    牛成民,2012.渤海南部海域莱州湾凹陷构造演化与油气成藏.石油与天然气地质,33(3):424-431.
    彭文绪,张如才,孙和风,等,2010.古新世以来郯庐断裂的位移量及其对莱州湾凹陷的控制.大地构造与成矿学,34(4):585-592.
    彭文绪,史浩,孙和风,等,2009a.郯庐走滑断层右旋走滑的地震切片证据.石油地球物理勘探,44(6):755-759,783,649.
    彭文绪,辛仁臣,孙和风,等,2009b.渤海海域莱州湾凹陷的形成和演化.石油学报,30(5):654-660.
    漆家福,2004.渤海湾新生代盆地的两种构造系统及其成因解释.中国地质,31(1):15-22.
    漆家福,周心怀,王谦身,2010.渤海海域中郯庐深断裂带的结构模型及新生代运动学.中国地质,37(5):1231-1242.
    漆家福,邓荣敬,周心怀,等,2008.渤海海域新生代盆地中的郯庐断裂带构造.中国科学:D辑,(S1):19-29.
    任建业,2004.渤海湾盆地东营凹陷S_(6')界面的构造变革意义.地球科学,(1):69-76,92.
    单家增,张占文,孙红军,等,2004.营口-佟二堡断裂带成因机制的构造物理模拟实验研究.石油勘探与开发,31(1):15-17.
    宋国奇,2006.郯庐断裂带鲁苏皖段大地电磁测深剖面与地壳结构.油气地质与采收率,13(6):1-4.
    孙和风,周心怀,彭文绪,等,2011.渤海南部黄河口凹陷晚期成藏特征及富集模式.石油勘探与开发,38(3):307-313.
    孙晓猛,王书琴,王英德,等,2010.郯庐断裂带北段构造特征及构造演化序列.岩石学报,26(1):165-176.
    索艳慧,李三忠,许立青,等,2015.渤海湾盆地大歧口凹陷新生代构造演化与盆地原型.地质科学,50(2):473-488.
    汤良杰,陈绪云,周心怀,等,2011.渤海海域郯庐断裂带构造解析.西南石油大学学报(自然科学版),33(1):170-176.
    童亨茂,宓荣三,于天才,等,2008.渤海湾盆地辽河西部凹陷的走滑构造作用.地质学报,82(8):1017-1026.
    万桂梅,汤良杰,周心怀,等,2010.渤海海域新近纪-第四纪断裂特征及形成机制.石油学报,31(4):591-595.
    万天丰,朱鸿,2002.中国大陆及邻区中生代-新生代大地构造与环境变迁.现代地质,16(2):107-120.
    王国纯,1998.郯庐断裂与渤海海域反转构造及花状构造.中国海上油气(地质),(5):1-7.
    吴福元,徐义刚,高山,等,2008.华北岩石圈减薄与克拉通破坏研究的主要学术争论.岩石学报,24(6):1145-1174.
    吴国强,吕修祥,周心怀,等,2013.新生代郯庐断裂活动在莱州湾地区的响应.石油实验地质,35(4):407-413.
    吴智平,侯旭波,李伟,2007.华北东部地区中生代盆地格局及演化过程探讨.大地构造与成矿学,31(4):385-399.
    徐佑德,柳忠泉,2006.郯庐断裂带营潍段走滑断裂特征.石油天然气学报,28(6):12-15.
    徐长贵,2016.渤海走滑转换带及其对大中型油气田形成的控制作用.地球科学,41(9):1548-1560.
    许立青,李三忠,索艳慧,等,2015.渤海湾盆地大歧口凹陷断裂系统与陆内拉分断陷.地质科学,50(2):489-502.
    严乐佳,2013.郯庐断裂带山东段新构造活动特征与动力学机制(硕士学位论文).合肥:合肥工业大学.
    张明振,付瑾平,印兴耀,2006.桩海地区的走滑和挤压构造特征.油气地质与采收率,13(2):5-7.
    张鹏,王良书,石火生,等,2010.郯庐断裂带山东段的中新生代构造演化特征.地质学报,84(9):1316-1323.
    张新涛,周心怀,牛成民,等,2014.渤海湾盆地黄河口凹陷油气成藏模式.石油天然气学报,36(3):30-36.
    张岳桥,董树文,2008.郯庐断裂带中生代构造演化史:进展与新认识.地质通报,27(9):1371-1390.
    周斌,邓志辉,晁洪太,等,2008.营潍断裂带走滑构造特征、演化及动力学机制.西北地震学报,30(2):117-123.
    周维维,王伟锋,安邦,等,2014.渤海湾盆地隐性断裂带识别及其地质意义.地球科学,39(11):1627-1638.
    朱光,王道轩,刘国生,等,2001.郯庐断裂带的伸展活动及其动力学背景.地质科学,36(3):269-278.
    朱光,王勇生,牛漫兰,等,2004.郯庐断裂带的同造山运动.地学前缘,11(3):169-182.
    朱光,徐佑德,刘国生,等,2006.郯庐断裂带中-南段走滑构造特征与变形规律.地质科学,41(2):226-241,255.
    朱秀香,吕修祥,王德英,等,2009.渤海海域黄河口凹陷走滑转换带对油气聚集的控制.石油与天然气地质,30(4):476-482.

© 2004-2018 中国地质图书馆版权所有 京ICP备05064691号 京公网安备11010802017129号

地址:北京市海淀区学院路29号 邮编:100083

电话:办公室:(+86 10)66554848;文献借阅、咨询服务、科技查新:66554700