营口—潍坊断裂带新生代运动学特征
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摘要
营口—潍坊断裂带在新生代时期对渤海湾盆地东部构造、沉积及油气成藏规律等方面具有重要影响和控制作用。依据大量实际地震资料,从剖面上识别出了花状构造、丝带效应、反转构造等营口—潍坊断裂带新生代时期走滑活动的标志,在平面上识别出了4种组合构造样式,在此基础上,应用拉分盆地走滑量计算的理论模型,对营口—潍坊断裂带新生代时期的走滑位移量进行了初步估算,认为营口—潍坊断裂带在新生代时期具右旋走滑活动特征,其主要走滑活动表现为3期,分别为始新世早期、渐新世早—中期和上新世晚期—第四纪,新生代累计右旋走滑位移量约为10～20km。
Evolution of the Yingkou-Weifang fault zone in Cenozoic is of great significance for us to study structure,sedimentaion,hydrocarbon generation and accumulation in east Bohai Bay basin.On the basis of the analysis from geophysics data,the author systematically studies structural styles of the Tan-Lu fault zone in Cenozoic.Six strike-slip marks and four combined structural styles were identified from seismic profiles and structural maps respectively.Yingkou-Weifang segment of the Tan-Lu fault zone is known to have experienced three main stages of dextral strike slide in Cenozoic through the comprehensive analysis,and the displacement of dextral strike-slip was 10～20 km.
Evolution of the Yingkou-Weifang fault zone in Cenozoic is of great significance for us to study structure,sedimentaion,hydrocarbon generation and accumulation in east Bohai Bay basin.On the basis of the analysis from geophysics data,the author systematically studies structural styles of the Tan-Lu fault zone in Cenozoic.Six strike-slip marks and four combined structural styles were identified from seismic profiles and structural maps respectively.Yingkou-Weifang segment of the Tan-Lu fault zone is known to have experienced three main stages of dextral strike slide in Cenozoic through the comprehensive analysis,and the displacement of dextral strike-slip was 10～20 km.
引文
[1]漆家福,陈发景.下辽河—辽东湾新生代裂陷盆地的构造解析[M].北京:地质出版社:1995a:44-53.[QI Jia-fu,CHEN Fa-jing.Tectonic Interpretation of Xialiaohe River-Liaodong Bay Cenozoic Rift Basin[M].Beijing:Geologic Publishing House,1995a:44-53.]
[2]刘和甫,夏义平,殷进垠,等.走滑造山带与盆地耦合机制[J].地学前缘,1999,6(3):121-132.[LI U He-fu,XI A Yi-ping,YI NJin-yin,et al.Strike-slip orogenic zone and basin coupling mechanism[J].Earth Science Frontiers,1999.6(3):121-132.]
[3]刘和甫,李晓清,刘立群,等.走滑构造体系盆山耦合与区带分析[J].现代地质,2004,18(2):139-150.[LI U He-fu,LI Xiao-qing,LI U Li-qun,et al.Analysis of strike-slip-type basin-mountain coupling and zoning[J].Geoscience,2004,18(2):139-150.]
[4]蔡东升,罗晖,武文来,等.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[J].中国海上油气地质,2001a,15(1):35-43.[CAI Dong-sheng,LUO Hui,WU Wen-lai,et al.Relation of shallowtectonic deformation and genetic mechanismin the Bohai Sea with Bozhong depression and the surrounding oil-gas enrichment[J].China Offshore Oil and Gas(Geology),2001a,15(1):35-43.]
[5]蔡东升,罗晖,姚长华.渤海莱州湾走滑拉分凹陷的构造研究及其石油勘探意义[J].石油学报,2001b,22(2):19-25.[CAIDong-sheng,LUO Hui,YAO Chang-hua.Tectonics and pe-troleumexplorationi mplication of strike-slip-pull-apart sags in Laizhou Bay of the Bohai Sea[J].Acta Petrolei Sinica,2001b,22(2):19-25.]
[6]Harding T P.Newport-Inglewood trend,California-an exam-ple of wrenching style of deformation[J].AAPG Bulletin,1973,57(1):97-116.
[7]Harding T P.Petroleumtraps associated with wrench faults[J].AAPG Bulletin,1974,58:1290-1304.
[8]Harding T P.Tectonic significance and hydrocarbon trapping consequences of sequential folding synchronous with San An-dreas faulting,San Joaquin Valley,California[J].AAPG Bul-letin,1976,58(7):356-378.
[9]Harding T P,Lowell J D.Structural styles,their plate-tec-tonic habitats,and hydrocarbon traps in petroleum provinces[J].AAPG Bulletin,1979,63(7):1016-1058.
[10]Harding T P.Seismic characteristics and identification of negative flower,positive flower structures and positive struc-tural inversion[J].AAPG Bulletin1985,69(4):582-600.
[11]Harding T P.Identification of wrench faults using subsurface structural data:criteria and pitfalls[J].AAPG Bulletin,1990,74(10):1590-1609.
[12]Sylvester A G.Compiler,wrench fault tectonics[J].Ameri-can Association of Petroleum Geologists Reprint,1984(28):374.
[13]Sylvester A G.Strikeslip faults[J].Geological Society of A-merica Bulletin,1988,100(11):1666-1703.
[14]蔡希源,王同和.中国含油气区反转构造[M].北京:石油工业出版社,2001:1-402.[CAI Xi-yuan,WANG Tong-he.Re-verse Structures of China Petroliferous Areas[M].Beijing:PetroleumIndustry Press,2001:1-402.]
[15]李晓清,汪泽成,程有义,等.拉分盆地分析与含油气性—以潍北盆地为例[M].山东东营:石油大学出版社,2003.[LI Xi-ao-qing,WANG Ze-cheng,CHENG You-yi,et al.Analysis of Pull-apart Basins and PetroleumProspect:Weibei Basin as an Example[M].Dongying:China University of Petroleum Press,2003.]
[16]Wilcox R E,Harding T P,Seely D R.Basic wrench tectonics[J].AAPG Bulletin,1973,57(1):74-96.
[17]Aydin A,Nur A.Evolution of pull-apart basins and their in-dependence[J].Tectonics,1982,1(1):91-105.
[18]Hempton M R,Neher K.Experi mental fracture,strain and subsidence patterns overnchelon strike-slip faults:i mplica-tions for the structural evolution of pull-apart basins[J].Journal of Structural Geology,1986,8(6):597-605.
[19]Woodcock N H.The role of strike-slip fault systems at plate boundaries[J].Royal Society of London Philosophical Trans-actions,1986,317(Series A):13-29.
[20]Woodcock N H,Fischer,M.Strike-slip duplexes[J].Jour-nal of Structural Geology,1986,8(7):725-735.
[21]Woodcock N H,Richards B.Transpressive duplex and flow-er structure:Dent Fault System,NWEngland[J].Journal of Structural Geology,2003,25(12):1981-1992.
[22]Xu J W,Zhu G,Tong WX,et al.Formation and evolution of the Tancheng-Lujiang wrenchfault systems:a major shear systemtothe northern of the Pacific Ocean[J].Tectonophys-ics,1987,134:273-310.
[23]Xu J W.The Tancheng-Lujiang Wrench Fault System[M].Chichester(UK):John Wiley&Sons Ltd.,1993:1-74.
[24]Xu J W,Zhu G.Tectonic models of the Tan-Lu fault zone,eastern China[J].International Geology Review,1994,36:771-784.
[25]环文林,汪素云,常向东,等.渤海地震活动特征[J].地震研究.1989,12(1):1-10.[HUAN Wen-lin,WANG Su-yun,CHANG Xiang-dong,et al.Characteristics of Bohai earth-quake activities[J].Journal of Seismological Research,1989,12(1):1-10.]
[26]Ben-avraham Z,Zoback M D.Transform-normal extension and asymmetric basins:an alternative to pull-apart models[J].Geology,1992,23(5):423-426.
[27]Wan T F.Evolution of Tancheng-Lujiang Fault Zone and Pa-leostress Fields[M].Press of China University of Geosci-ences,1995a:26-42.
[28]Wan T F.Length and Penetration Depth of the Tancheng-Lujiang Fault Zone[M].Press of China University of Geosci-ences,1995b:12-25.
[29]Wan T F.Forming and Evolution of the Tancheng-Lujiang Fault Zone in Eastern Asia[M].Press of China University of Geosciences,1995c:1-11.
[30]Wan T F.The Maxi mum Sinistral Strike-Slip and Its Form-ing Stage for Tancheng-Lujiang Fault Zone[M].Press of China University of Geosciences,1995d:62-76.
[31]徐嘉炜.论走滑断层作用的几个问题[J].地学前缘,1995a,2(1-2):125-136.[XUJia-wei.On some problems about strike-slip faulting[J].Earth Science Frontiers,1995a,2(1-2):125-136.]
[32]徐嘉炜,朱光.中国东部郯庐断裂带构造模式讨论[J].华北地质矿产杂志,1995b,10(2):121-134.[XU Jia-wei,ZHU Guang.Discussion on tectonic model for Tan-Lu fracture zone in eastern China[J].Journal of Geology and Mineral Re-sources of North China,1995b,10(2):121-134.]
[33]徐嘉炜,朱光,吕培基,等.郯庐断裂带平移的年代学研究进展[J].安徽地质,1995c,5(1):1-12.[XU Jia-wei,ZHU Guang,L Pei-ji,et al.Chronology of Tan-Lufracture zone strike-slip activity[J].Geology of Anhui,1995c,5(1):1-12.]
[34]董旭光,周蕈英,华爱军.渤海海峡及邻区现代小震震源机制分析[J].内陆地震,1999,13(1):7-16.[DONG Xu-guang,ZHOU Qin-ying,HUA Ai-jun.Analysis of modern focal mechanismof small earthquakes in Bohai Strait and adjacent areas[J].Inland Earthquake,1999,13(1):7-16.]
[35]王小凤,李中坚,陈柏林,等.郯庐断裂带[J].北京:地质出版社,2000:1-200.[WANG Xiao-feng,LI Zhong-jian,CHEN Bai-lin,et al.Tan-Lu Fracture Zone[M].Beijing:Geologic Publishing House,2000:1-200.]
[36]Allen P A,Allen J R.Basin Analysis-Principles andApp1ications[M].BIackwell Scientific Publication,2005:190-218.
[37]万天丰.郯庐断裂带的演化与古应力场[J].地球科学—中国地质大学学报,1995,20(5):526-533.[WAN Tian-feng.Evo-lution of Tan-Lu fracture zone and ancient stress field[J].Journal of China University of Geosciences(Earth Science),1995,20(5):526-533.]
[38]陈丕基.郯庐断裂巨大平移的时代与格局[J].科学通报,1988,33(4):289-293.[CHEN Pi-ji.Ti mes and pattern of great strike-slip activity of Tan-Lu fracture zone[J].Chinese Science Bulletin,1988,33(4):289-293.]
[39]李玉喜,罗笃清,云金表.走滑构造变形量估算方法探讨[J].石油勘探与开发,1995,22(1):13-15.[LI Yu-xi,LUO Du-qing,YUNJin-biao.Methods for esti mation of strike-slip de-formation[J].Petroleum Exploration and Development,1995,22(1):13-15.]
[40]李三忠,周立宏,刘建忠,等.华北板块东部新生代断裂构造特征与盆地成因[J].海洋地质与第四纪地质,2004,24(3):57-66.[LI San-zhong,ZHOU Li-hong,LI U Jian-zhong,et al.Cenozoic faulting characteristics and basin genesis in the east of North China block[J].Marine Geology and Quaterna-ry Geology,2004,24(3):57-66.]
[41]岳云福,李三忠,郝德峰,等.张性环境中与断裂相关的褶皱类型及特征[J].青岛海洋大学学报,2003,33(4):574-580.[YUE Yun-fu,LI San-zhong,HAO De-feng,et al.Types and characteristics of folds related to faults in extensional en-vironment[J].Journal of Ocean University of Qingdao,2003,33(4):574-580.]
[42]王光奇,李三忠,周立宏,等.张东断层成因机制与油气关系[J].石油勘探与开发,2002,29(6):38-40.[WANG Guang-qi,LI San-zhong,ZHOU Li-hong,et al.Genetic mechanism of Zhangdongfault andits relation with petroleum[J].Petro-leum Exploration and Development,2002,29(6):38-40.]
[2]刘和甫,夏义平,殷进垠,等.走滑造山带与盆地耦合机制[J].地学前缘,1999,6(3):121-132.[LI U He-fu,XI A Yi-ping,YI NJin-yin,et al.Strike-slip orogenic zone and basin coupling mechanism[J].Earth Science Frontiers,1999.6(3):121-132.]
[3]刘和甫,李晓清,刘立群,等.走滑构造体系盆山耦合与区带分析[J].现代地质,2004,18(2):139-150.[LI U He-fu,LI Xiao-qing,LI U Li-qun,et al.Analysis of strike-slip-type basin-mountain coupling and zoning[J].Geoscience,2004,18(2):139-150.]
[4]蔡东升,罗晖,武文来,等.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[J].中国海上油气地质,2001a,15(1):35-43.[CAI Dong-sheng,LUO Hui,WU Wen-lai,et al.Relation of shallowtectonic deformation and genetic mechanismin the Bohai Sea with Bozhong depression and the surrounding oil-gas enrichment[J].China Offshore Oil and Gas(Geology),2001a,15(1):35-43.]
[5]蔡东升,罗晖,姚长华.渤海莱州湾走滑拉分凹陷的构造研究及其石油勘探意义[J].石油学报,2001b,22(2):19-25.[CAIDong-sheng,LUO Hui,YAO Chang-hua.Tectonics and pe-troleumexplorationi mplication of strike-slip-pull-apart sags in Laizhou Bay of the Bohai Sea[J].Acta Petrolei Sinica,2001b,22(2):19-25.]
[6]Harding T P.Newport-Inglewood trend,California-an exam-ple of wrenching style of deformation[J].AAPG Bulletin,1973,57(1):97-116.
[7]Harding T P.Petroleumtraps associated with wrench faults[J].AAPG Bulletin,1974,58:1290-1304.
[8]Harding T P.Tectonic significance and hydrocarbon trapping consequences of sequential folding synchronous with San An-dreas faulting,San Joaquin Valley,California[J].AAPG Bul-letin,1976,58(7):356-378.
[9]Harding T P,Lowell J D.Structural styles,their plate-tec-tonic habitats,and hydrocarbon traps in petroleum provinces[J].AAPG Bulletin,1979,63(7):1016-1058.
[10]Harding T P.Seismic characteristics and identification of negative flower,positive flower structures and positive struc-tural inversion[J].AAPG Bulletin1985,69(4):582-600.
[11]Harding T P.Identification of wrench faults using subsurface structural data:criteria and pitfalls[J].AAPG Bulletin,1990,74(10):1590-1609.
[12]Sylvester A G.Compiler,wrench fault tectonics[J].Ameri-can Association of Petroleum Geologists Reprint,1984(28):374.
[13]Sylvester A G.Strikeslip faults[J].Geological Society of A-merica Bulletin,1988,100(11):1666-1703.
[14]蔡希源,王同和.中国含油气区反转构造[M].北京:石油工业出版社,2001:1-402.[CAI Xi-yuan,WANG Tong-he.Re-verse Structures of China Petroliferous Areas[M].Beijing:PetroleumIndustry Press,2001:1-402.]
[15]李晓清,汪泽成,程有义,等.拉分盆地分析与含油气性—以潍北盆地为例[M].山东东营:石油大学出版社,2003.[LI Xi-ao-qing,WANG Ze-cheng,CHENG You-yi,et al.Analysis of Pull-apart Basins and PetroleumProspect:Weibei Basin as an Example[M].Dongying:China University of Petroleum Press,2003.]
[16]Wilcox R E,Harding T P,Seely D R.Basic wrench tectonics[J].AAPG Bulletin,1973,57(1):74-96.
[17]Aydin A,Nur A.Evolution of pull-apart basins and their in-dependence[J].Tectonics,1982,1(1):91-105.
[18]Hempton M R,Neher K.Experi mental fracture,strain and subsidence patterns overnchelon strike-slip faults:i mplica-tions for the structural evolution of pull-apart basins[J].Journal of Structural Geology,1986,8(6):597-605.
[19]Woodcock N H.The role of strike-slip fault systems at plate boundaries[J].Royal Society of London Philosophical Trans-actions,1986,317(Series A):13-29.
[20]Woodcock N H,Fischer,M.Strike-slip duplexes[J].Jour-nal of Structural Geology,1986,8(7):725-735.
[21]Woodcock N H,Richards B.Transpressive duplex and flow-er structure:Dent Fault System,NWEngland[J].Journal of Structural Geology,2003,25(12):1981-1992.
[22]Xu J W,Zhu G,Tong WX,et al.Formation and evolution of the Tancheng-Lujiang wrenchfault systems:a major shear systemtothe northern of the Pacific Ocean[J].Tectonophys-ics,1987,134:273-310.
[23]Xu J W.The Tancheng-Lujiang Wrench Fault System[M].Chichester(UK):John Wiley&Sons Ltd.,1993:1-74.
[24]Xu J W,Zhu G.Tectonic models of the Tan-Lu fault zone,eastern China[J].International Geology Review,1994,36:771-784.
[25]环文林,汪素云,常向东,等.渤海地震活动特征[J].地震研究.1989,12(1):1-10.[HUAN Wen-lin,WANG Su-yun,CHANG Xiang-dong,et al.Characteristics of Bohai earth-quake activities[J].Journal of Seismological Research,1989,12(1):1-10.]
[26]Ben-avraham Z,Zoback M D.Transform-normal extension and asymmetric basins:an alternative to pull-apart models[J].Geology,1992,23(5):423-426.
[27]Wan T F.Evolution of Tancheng-Lujiang Fault Zone and Pa-leostress Fields[M].Press of China University of Geosci-ences,1995a:26-42.
[28]Wan T F.Length and Penetration Depth of the Tancheng-Lujiang Fault Zone[M].Press of China University of Geosci-ences,1995b:12-25.
[29]Wan T F.Forming and Evolution of the Tancheng-Lujiang Fault Zone in Eastern Asia[M].Press of China University of Geosciences,1995c:1-11.
[30]Wan T F.The Maxi mum Sinistral Strike-Slip and Its Form-ing Stage for Tancheng-Lujiang Fault Zone[M].Press of China University of Geosciences,1995d:62-76.
[31]徐嘉炜.论走滑断层作用的几个问题[J].地学前缘,1995a,2(1-2):125-136.[XUJia-wei.On some problems about strike-slip faulting[J].Earth Science Frontiers,1995a,2(1-2):125-136.]
[32]徐嘉炜,朱光.中国东部郯庐断裂带构造模式讨论[J].华北地质矿产杂志,1995b,10(2):121-134.[XU Jia-wei,ZHU Guang.Discussion on tectonic model for Tan-Lu fracture zone in eastern China[J].Journal of Geology and Mineral Re-sources of North China,1995b,10(2):121-134.]
[33]徐嘉炜,朱光,吕培基,等.郯庐断裂带平移的年代学研究进展[J].安徽地质,1995c,5(1):1-12.[XU Jia-wei,ZHU Guang,L Pei-ji,et al.Chronology of Tan-Lufracture zone strike-slip activity[J].Geology of Anhui,1995c,5(1):1-12.]
[34]董旭光,周蕈英,华爱军.渤海海峡及邻区现代小震震源机制分析[J].内陆地震,1999,13(1):7-16.[DONG Xu-guang,ZHOU Qin-ying,HUA Ai-jun.Analysis of modern focal mechanismof small earthquakes in Bohai Strait and adjacent areas[J].Inland Earthquake,1999,13(1):7-16.]
[35]王小凤,李中坚,陈柏林,等.郯庐断裂带[J].北京:地质出版社,2000:1-200.[WANG Xiao-feng,LI Zhong-jian,CHEN Bai-lin,et al.Tan-Lu Fracture Zone[M].Beijing:Geologic Publishing House,2000:1-200.]
[36]Allen P A,Allen J R.Basin Analysis-Principles andApp1ications[M].BIackwell Scientific Publication,2005:190-218.
[37]万天丰.郯庐断裂带的演化与古应力场[J].地球科学—中国地质大学学报,1995,20(5):526-533.[WAN Tian-feng.Evo-lution of Tan-Lu fracture zone and ancient stress field[J].Journal of China University of Geosciences(Earth Science),1995,20(5):526-533.]
[38]陈丕基.郯庐断裂巨大平移的时代与格局[J].科学通报,1988,33(4):289-293.[CHEN Pi-ji.Ti mes and pattern of great strike-slip activity of Tan-Lu fracture zone[J].Chinese Science Bulletin,1988,33(4):289-293.]
[39]李玉喜,罗笃清,云金表.走滑构造变形量估算方法探讨[J].石油勘探与开发,1995,22(1):13-15.[LI Yu-xi,LUO Du-qing,YUNJin-biao.Methods for esti mation of strike-slip de-formation[J].Petroleum Exploration and Development,1995,22(1):13-15.]
[40]李三忠,周立宏,刘建忠,等.华北板块东部新生代断裂构造特征与盆地成因[J].海洋地质与第四纪地质,2004,24(3):57-66.[LI San-zhong,ZHOU Li-hong,LI U Jian-zhong,et al.Cenozoic faulting characteristics and basin genesis in the east of North China block[J].Marine Geology and Quaterna-ry Geology,2004,24(3):57-66.]
[41]岳云福,李三忠,郝德峰,等.张性环境中与断裂相关的褶皱类型及特征[J].青岛海洋大学学报,2003,33(4):574-580.[YUE Yun-fu,LI San-zhong,HAO De-feng,et al.Types and characteristics of folds related to faults in extensional en-vironment[J].Journal of Ocean University of Qingdao,2003,33(4):574-580.]
[42]王光奇,李三忠,周立宏,等.张东断层成因机制与油气关系[J].石油勘探与开发,2002,29(6):38-40.[WANG Guang-qi,LI San-zhong,ZHOU Li-hong,et al.Genetic mechanism of Zhangdongfault andits relation with petroleum[J].Petro-leum Exploration and Development,2002,29(6):38-40.]
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