黄骅坳陷南部滩海区中生界构造与演化
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摘要
渤海湾盆地区中生界构造演化与样式始终不明朗,中生代该区处于整个华北克拉通东部高原的核心部位。其构造演化研究对深入理解这个高原从形成至垮塌的过程至关重要。同时,中生界也是近年来中国东部深部油气勘探的主要目标。黄骅坳陷南部滩海区不仅是大港探区中生界潜山油气的重要勘探区,而且处于渤海湾盆地中新生代构造格局转换部位,具有重要研究价值。利用大量地震剖面,系统进行了中生界残存展布规律的分析,进一步划分了该区构造单元,探讨了该区中生界构造演化过程。特别是,以羊二庄断层为界,研究区可以分为两个构造区,东南区构造相对简单;西北区构造复杂,既继承了印支期东西向构造格局,又经历燕山早、中期走滑挤压和燕山晚期及新生代的伸展走滑,还产生了强烈的滑断构造。羊二庄断层是在印支期构造的基础上发展起来的一组剪切断裂,在燕山中期经历了挤压走滑,在燕山晚期和新生代经历右行伸展运动而形成的呈NE向的复杂断层系。可见羊二庄断层的演化控制了该区中生界的构造格局和演化。
Bohai Bay basin range is located at the center of a Mesozoic plateau in eastern North China craton in Mesozoic.Its structural evolution is a key problem to understand process from formation to collapse of this plateau.Moreover,these Mesozoic strata are important oil-gas exploration objectives in eastern China in recent years.However,structural pattern and evolution of this region are not clear up to the present.The south shore of Huanghua depression is not only an important and new oil-gas exploration area for Mesozoic buried hill in the Dagang exploration area,but also is located at spatial and temperal switch site of Mesozoic-Cenozoic structural patterns of the Bohai Bay basin.Therefore,the study area is of important implication for research.A large number of seismic profiles were interpreted to analyze distribution rule of relic Mesozoic strata.Furthermore,we subdivided the structural units in the study area and discussed its Mesozoic structural evolution.Taking Yang'erzhuang fault as a border,we divided the study area into a northwest region and a southeast region. Structures in the former is more complex than in the latter.The northwest region inherited EW Indosinian structural pattern,and also experienced slip and compression during the early and middle Yanshan movement.Then strike-slip and intense slip-break structures occurred during Yanshan movement and Cenozoic.The Yang'erzhuang fault is a strike-slip fault system which evolved from Indosinian period and then experienced compression and strike slipping in middle Yanshan movement,and went through dextral slipping during Yanshan movement and Cenozoic.These processes indicate that the Yang'erzhuang fault controls the structural pattern and evolution of Mesozoic strata in this area.In summery,structural evolution in the study area is an epitome of tectonic evolution of the Bohai Bay basin.
Bohai Bay basin range is located at the center of a Mesozoic plateau in eastern North China craton in Mesozoic.Its structural evolution is a key problem to understand process from formation to collapse of this plateau.Moreover,these Mesozoic strata are important oil-gas exploration objectives in eastern China in recent years.However,structural pattern and evolution of this region are not clear up to the present.The south shore of Huanghua depression is not only an important and new oil-gas exploration area for Mesozoic buried hill in the Dagang exploration area,but also is located at spatial and temperal switch site of Mesozoic-Cenozoic structural patterns of the Bohai Bay basin.Therefore,the study area is of important implication for research.A large number of seismic profiles were interpreted to analyze distribution rule of relic Mesozoic strata.Furthermore,we subdivided the structural units in the study area and discussed its Mesozoic structural evolution.Taking Yang'erzhuang fault as a border,we divided the study area into a northwest region and a southeast region. Structures in the former is more complex than in the latter.The northwest region inherited EW Indosinian structural pattern,and also experienced slip and compression during the early and middle Yanshan movement.Then strike-slip and intense slip-break structures occurred during Yanshan movement and Cenozoic.The Yang'erzhuang fault is a strike-slip fault system which evolved from Indosinian period and then experienced compression and strike slipping in middle Yanshan movement,and went through dextral slipping during Yanshan movement and Cenozoic.These processes indicate that the Yang'erzhuang fault controls the structural pattern and evolution of Mesozoic strata in this area.In summery,structural evolution in the study area is an epitome of tectonic evolution of the Bohai Bay basin.
引文
[1]刘建忠,李三忠,周立宏,等.华北板块东部中生代构造演化与盆地格局[J].海洋地质与第四纪地质,2004,24(4):45-54.[LIU Jian-zhong,LI San-zhong,ZHOU Li-hong,et al.Mesozo-ic tectonic and basin distribution in the eastern North ChinaPlate[J].Marine Geology and Quaternary Geology,2004,24(4):45-54.]
[2]周立宏,李三忠,赵国春,等.华北克拉通中东部基底构造单元的重磁特征[J].地球物理学进展,2004,19(1):91-100.[ZHOU Li-hong,LI San-zhong,ZHAO Guo-chun,et al.Gravity and magnetic features of crystalline basement in thecentral and Eastern North China Craton[J],Progress in Geo-physics,2004,19(1):91-100.]
[3]LI San-zhong,XU Shu-mei,SHAN Ye-hua,et al.Tectonic e-volution and basin assemblage in the Bohai Bay and its neigh-bors[J].Acta Oceanologica Sinica,2000(4):91-106.
[4]李三忠,许淑梅,单业华,等.渤海湾及邻区构造演化与盆地组合规律[J].海洋学报,2000,22(增刊):220-229.[LI San-zhong,XU Shu-mei,SHAN Ye-hua,et al.Tectonic evolutionand basin assemblage in the Bohai Bay and its neighbors[J].Acta Oceanologica Sinica,2000,22(Supplement):220-229]
[5]李三忠,王金铎,刘建忠,等.鲁西地块中生代挤压构造格局及其形成背景[J].地质学报,2005,79(4):487-497.[LI San-zhong,WANG Jin-duo,LIU Jian-zhong,et al.Mesozoic struc-ture and its tectonic setting in the western Shandong block[J],Acta Geologica Sinica,2005,79(4):487-497.]
[6]侯方辉,李三忠,张志.济阳坳陷郭局子地区古潜山构造及储层特征[J].海洋地质动态,2005,21(8):24-47.[HOUFang-hui,LI San-zhong,ZHANG Zhi-xun,Tectonic and res-ervoir feature of ancient buried hills in Guojuzi area of Jiyangdepression[J],Marine Geology Letters,2005,21(8):24-47.]
[7]侯方辉,李三忠,王金铎,等.济阳坳陷桩海地区古潜山断裂[J].海洋地质与第四纪地质,2005,25(3):69-74.[HOUFang-hui,LI San-zhong,WANG Jin-duo,et al.Fault featureof buried hills at Zhuanghai,Jiyang depression[J].Marine Ge-ology and Quaternary Geology,2005,25(3):69-74.]
[8]李三忠,刘建忠,赵国春,等.华北克拉通东部地块中生代变形的关键时限及其对构造的制约———以胶辽地区为例[J].岩石学报,2004,20(3):633-646.[LI San-zhong,LIU Jian-zhong,ZHAO Guo-chun,et al.Key geochronology of Mesozoic de-formation in the eastern block of the North China Craton andits constraints on regional tectonics:a case of Jiaodong and Lia-odong Peninsula[J].Acta Petrologica Sinica,2004,20(3):633-646.]
[9]吴福元,葛文春,孙德有,等.中国东部岩石圈减薄研究中的几个问题[J].地学前缘,2003,10(3):51-60.[WU Fu-yuan,GE Wen-chun,SUN De-you,et al.Discussion on the lithos-pheric thinning in Eastern China[J].Earth Science Frontiers.2003,10(3):51-60.]
[10]张旗,钱青,王二七,等.燕山中晚期的中国东部高原:埃达克岩的启示[J].地质科学,2001,36(2):248-255.[ZHANG Qi,QIAN Qing,WANG Er-qi,et al.An east Chi-na plateau in Mid-Late Yanshanian[J].Scientia GeologicaSinica.2001,36(2):248-255.]
[11]王光奇,李三忠,周立宏.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.Relation between pe-troleum accumulation and genetic mechanism of Zhangdongfault in Huanghua depression[J].Petrdeum Exploration andDevelopment,2002,29(6):38-40.]
[12]YU Jian-guo,LI San-zhong,WANG Jin-duo,et al.Salt dia-pirism and faulting of the Central Uplift Belt in the DongyingSag of the Bohai Bay Basin,North China[J].Acta Oceanologi-ca Sinica,2005,24(2):28-42.
[13]于建国,李三忠,王金铎,等.东营凹陷泥岩底辟作用与中央隆起带断裂成因[J].地质科学,2005,40(1):55-68.[YUJian-guo,LI San-zhong,WANG Jin-duo,et al.Salt diapirismand faulting of the Central Uplift Belt in the Dongying Sag,Bohai Bay Basin,North China[J].Chinese Journal of Geolo-gy,2005,40(1):55-68.]
[14]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,LIU Jian-zhong,etal.Cenozoic faulting and basin formation in the EasternNorth China Plate[J].Marine Geology and Quaternary Geol-ogy,2004,24(3):57-66.]
[15]漆家福,于福生,陆克政,等.渤海湾地区的中生代盆地构造概论[J].地学前缘,2003,10(特刊):199-205.[QI Jia-fu,YUFu-sheng,LU Ke-zheng,et al.Conspectus on Mesozoic ba-sins in Bohai Bay Province[J].Earth Science Frontiers,2003,10(Special issue):199-205.]
[16]中国地质调查局古生物研究中心.中国各地质时代地层划分与对比[M].北京,地质出版社,2005.[Center for Stratigra-phy and Palaeontology,China Geological Survey.Stratigra-phy Division and Correlation of Each Geologic Period in China[M].Beijing:Geologic Publishing House,2005.]
[17]杜旭东,漆家福,陆克政,等.大港探区中生代盆地构造特征及演化[J].石油实验地质,2000,22(2):125-130.[DU Xu-dong,QI Jia-fu,LU Ke-zheng,et al.Evolution and Tectoniccharacteristics of the Mesozoic Basin in Dagang Prospect Area[J].Experimental Petroleum Geology,2000,22(2):125-130.]
[18]杨池银.大港探区领域及对策分析[J].中国石油勘探,2003,8(2):13-17.[YANG Chi-yin.Exploration realm and strate-gy analysis for Dagang Exploration Area[J].China Petrole-um Exploration,2003,8(2):13-17.]
[19]于福生,漆家福,王春英.华北东部印支期构造变形研究[J].中国矿业大学学报,2002,31(4):402-405.[YU Fu-sheng,QIJia-fu,WANG Chun-ying.Tectonic deformation of Indosinianperiod in eastern part of North China[J].Journal of China U-niversity of Mining and Technology,2002,31(4):402-405.]
[20]吴永平,付立新,杨池银,等.黄骅坳陷中生代构造演化对潜山油气成藏的影响[J].石油学报,2002,23(2):16-21.[WUYong-ping,FU Li-xin,YANG Chi-yin,et al.Huanghua De-pression buried hill Mesozoic tectonic hydrocarbon accumula-tion[J].Acta Petrolei Sinica,2002,23(2):16-21.]
[21]王光奇,漆家福,岳云福.歧口凹陷及周缘新生代构造的成因和演化[J].地质科学,2003,38(2):230-240.[WANGGuang-qi,QI Jia-fu,YUE Yun-fu.Formation and evolution ofthe Cenozoic tectonics and surrounding the Qikou Sag[J].Chinese Journal of Geology,2003,38(2):230-240.]
[22]周立宏,李三忠,刘建忠,等.渤海湾盆地区燕山期构造特征与原型盆地[J].地球物理学进展,2003,18(4):692-699.[ZHOU Li-hong,LI San-zhong,LIU Jian-zhong,et al.TheYanshanian structural style and basin prototypes of the Meso-zoic Bohai Bay Basin[J].Progress in Geophysics,2003,18(4):692-699.]
[2]周立宏,李三忠,赵国春,等.华北克拉通中东部基底构造单元的重磁特征[J].地球物理学进展,2004,19(1):91-100.[ZHOU Li-hong,LI San-zhong,ZHAO Guo-chun,et al.Gravity and magnetic features of crystalline basement in thecentral and Eastern North China Craton[J],Progress in Geo-physics,2004,19(1):91-100.]
[3]LI San-zhong,XU Shu-mei,SHAN Ye-hua,et al.Tectonic e-volution and basin assemblage in the Bohai Bay and its neigh-bors[J].Acta Oceanologica Sinica,2000(4):91-106.
[4]李三忠,许淑梅,单业华,等.渤海湾及邻区构造演化与盆地组合规律[J].海洋学报,2000,22(增刊):220-229.[LI San-zhong,XU Shu-mei,SHAN Ye-hua,et al.Tectonic evolutionand basin assemblage in the Bohai Bay and its neighbors[J].Acta Oceanologica Sinica,2000,22(Supplement):220-229]
[5]李三忠,王金铎,刘建忠,等.鲁西地块中生代挤压构造格局及其形成背景[J].地质学报,2005,79(4):487-497.[LI San-zhong,WANG Jin-duo,LIU Jian-zhong,et al.Mesozoic struc-ture and its tectonic setting in the western Shandong block[J],Acta Geologica Sinica,2005,79(4):487-497.]
[6]侯方辉,李三忠,张志.济阳坳陷郭局子地区古潜山构造及储层特征[J].海洋地质动态,2005,21(8):24-47.[HOUFang-hui,LI San-zhong,ZHANG Zhi-xun,Tectonic and res-ervoir feature of ancient buried hills in Guojuzi area of Jiyangdepression[J],Marine Geology Letters,2005,21(8):24-47.]
[7]侯方辉,李三忠,王金铎,等.济阳坳陷桩海地区古潜山断裂[J].海洋地质与第四纪地质,2005,25(3):69-74.[HOUFang-hui,LI San-zhong,WANG Jin-duo,et al.Fault featureof buried hills at Zhuanghai,Jiyang depression[J].Marine Ge-ology and Quaternary Geology,2005,25(3):69-74.]
[8]李三忠,刘建忠,赵国春,等.华北克拉通东部地块中生代变形的关键时限及其对构造的制约———以胶辽地区为例[J].岩石学报,2004,20(3):633-646.[LI San-zhong,LIU Jian-zhong,ZHAO Guo-chun,et al.Key geochronology of Mesozoic de-formation in the eastern block of the North China Craton andits constraints on regional tectonics:a case of Jiaodong and Lia-odong Peninsula[J].Acta Petrologica Sinica,2004,20(3):633-646.]
[9]吴福元,葛文春,孙德有,等.中国东部岩石圈减薄研究中的几个问题[J].地学前缘,2003,10(3):51-60.[WU Fu-yuan,GE Wen-chun,SUN De-you,et al.Discussion on the lithos-pheric thinning in Eastern China[J].Earth Science Frontiers.2003,10(3):51-60.]
[10]张旗,钱青,王二七,等.燕山中晚期的中国东部高原:埃达克岩的启示[J].地质科学,2001,36(2):248-255.[ZHANG Qi,QIAN Qing,WANG Er-qi,et al.An east Chi-na plateau in Mid-Late Yanshanian[J].Scientia GeologicaSinica.2001,36(2):248-255.]
[11]王光奇,李三忠,周立宏.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.Relation between pe-troleum accumulation and genetic mechanism of Zhangdongfault in Huanghua depression[J].Petrdeum Exploration andDevelopment,2002,29(6):38-40.]
[12]YU Jian-guo,LI San-zhong,WANG Jin-duo,et al.Salt dia-pirism and faulting of the Central Uplift Belt in the DongyingSag of the Bohai Bay Basin,North China[J].Acta Oceanologi-ca Sinica,2005,24(2):28-42.
[13]于建国,李三忠,王金铎,等.东营凹陷泥岩底辟作用与中央隆起带断裂成因[J].地质科学,2005,40(1):55-68.[YUJian-guo,LI San-zhong,WANG Jin-duo,et al.Salt diapirismand faulting of the Central Uplift Belt in the Dongying Sag,Bohai Bay Basin,North China[J].Chinese Journal of Geolo-gy,2005,40(1):55-68.]
[14]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,LIU Jian-zhong,etal.Cenozoic faulting and basin formation in the EasternNorth China Plate[J].Marine Geology and Quaternary Geol-ogy,2004,24(3):57-66.]
[15]漆家福,于福生,陆克政,等.渤海湾地区的中生代盆地构造概论[J].地学前缘,2003,10(特刊):199-205.[QI Jia-fu,YUFu-sheng,LU Ke-zheng,et al.Conspectus on Mesozoic ba-sins in Bohai Bay Province[J].Earth Science Frontiers,2003,10(Special issue):199-205.]
[16]中国地质调查局古生物研究中心.中国各地质时代地层划分与对比[M].北京,地质出版社,2005.[Center for Stratigra-phy and Palaeontology,China Geological Survey.Stratigra-phy Division and Correlation of Each Geologic Period in China[M].Beijing:Geologic Publishing House,2005.]
[17]杜旭东,漆家福,陆克政,等.大港探区中生代盆地构造特征及演化[J].石油实验地质,2000,22(2):125-130.[DU Xu-dong,QI Jia-fu,LU Ke-zheng,et al.Evolution and Tectoniccharacteristics of the Mesozoic Basin in Dagang Prospect Area[J].Experimental Petroleum Geology,2000,22(2):125-130.]
[18]杨池银.大港探区领域及对策分析[J].中国石油勘探,2003,8(2):13-17.[YANG Chi-yin.Exploration realm and strate-gy analysis for Dagang Exploration Area[J].China Petrole-um Exploration,2003,8(2):13-17.]
[19]于福生,漆家福,王春英.华北东部印支期构造变形研究[J].中国矿业大学学报,2002,31(4):402-405.[YU Fu-sheng,QIJia-fu,WANG Chun-ying.Tectonic deformation of Indosinianperiod in eastern part of North China[J].Journal of China U-niversity of Mining and Technology,2002,31(4):402-405.]
[20]吴永平,付立新,杨池银,等.黄骅坳陷中生代构造演化对潜山油气成藏的影响[J].石油学报,2002,23(2):16-21.[WUYong-ping,FU Li-xin,YANG Chi-yin,et al.Huanghua De-pression buried hill Mesozoic tectonic hydrocarbon accumula-tion[J].Acta Petrolei Sinica,2002,23(2):16-21.]
[21]王光奇,漆家福,岳云福.歧口凹陷及周缘新生代构造的成因和演化[J].地质科学,2003,38(2):230-240.[WANGGuang-qi,QI Jia-fu,YUE Yun-fu.Formation and evolution ofthe Cenozoic tectonics and surrounding the Qikou Sag[J].Chinese Journal of Geology,2003,38(2):230-240.]
[22]周立宏,李三忠,刘建忠,等.渤海湾盆地区燕山期构造特征与原型盆地[J].地球物理学进展,2003,18(4):692-699.[ZHOU Li-hong,LI San-zhong,LIU Jian-zhong,et al.TheYanshanian structural style and basin prototypes of the Meso-zoic Bohai Bay Basin[J].Progress in Geophysics,2003,18(4):692-699.]
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