渤海海域西南部中生代构造演化过程与潜山形成机制
|
摘要
渤海湾盆地渤海海域西南部中生代潜山构造广泛发育,但对其成因演化机制尚缺乏系统的研究。为此,基于对该区三维地震资料的精细地层解释和构造样式识别,厘清断裂的期次、类型、活动特征,揭示关键构造期构造格局和潜山形成演化过程,明确潜山分带差异构造特征,并开展潜山类型划分。研究结果表明:①渤海海域西南部潜山内幕主要发育印支期、燕山早期、燕山中期、喜马拉雅期等4期构造运动,其中印支期、燕山早期构造运动对潜山形成和分布起到决定性的控制作用;②上述4期构造运动形成了由北东向、北西向和近南北向等3组断裂组成的4套复杂网格状断裂系统,各组断裂形成期次、性质及活动特征差异明显;③该区经历了古生代潜山物质基础形成、中生代晚三叠世—早侏罗世挤压造山与逆冲构造发育、晚侏罗世—早白垩世陆内裂陷及潜山初始格局的形成、新生代走滑—伸展复合改造与埋藏定型等4个演化阶段;④关键构造期表现形式的差异导致该区潜山构造特征呈现明显的分带性,可划分为西侧残留逆冲型潜山带、中部反转翘倾型潜山带和东侧复杂走滑断块型潜山带。结论认为,中、新生代经历多旋回的构造运动导致了该区潜山类型的多样性和内幕断裂系统的复杂性。
Mesozoic buried hill structures are widely developed in the southwestern Bohai Sea area of the Bohai Bay Basin, but the mechanisms of their genesis and evolution have not been systematically studied. In regard of this, the periods, types and activity characteristics of the faults in this area were analyzed based on the fine stratigraphic interpretation of three-dimensional seismic data and the identification of tectonic styles. Then, the tectonic framework in the key tectonic periods and the formation and evolution process of buried hills were revealed. Finally, the structural characteristics of different zones of buried hills were investigated and the buried hills were classified. And the following research results were obtained. First, there are four stages of tectonic movements inside the buried hills, including Indosinian, early Yanshanian, middle Yanshanian and Himalayan, among which Indosinian and early Yanshanian tectonic movements play a decisive role in controlling the formation and distribution of buried hills. Second, the four stages of tectonic movements formed four sets of complex grid-like fault systems consisting of three groups of faults(i.e. NE, NW and nearly NS faults), which are obviously different from each other in terms of formation stages, natures and activity characteristics. Third, the evolution of this area is divided into four stages, i.e., the formation of material base of buried hills in Paleozoic, the compressive orogeny and the thrust structure development in Late Triassic–Early Jurassic, the intracontinental rift and the formation of buried hill initial patterns in Late Jurassic–Early Cretaceous,and the strike-slip-extension composite transformation and the burial finalization in Cenozoic. Fourth, due to the differences of the manifestations of key tectonic periods, the structural characteristics of the buried hills in this area are obviously zonal, and they are divided into the residual thrust buried hill belt in the west, the inversion tilt buried hill belt in the central area and the complex strike-slip fault block buried hill belt in the east. It is concluded that the Mesozoic and Cenozoic strata in the southwestern Bohai Sea area undergo multicyclic tectonic movements, which result in the diversity of buried hill types and the complexity of the inner fault systems.
Mesozoic buried hill structures are widely developed in the southwestern Bohai Sea area of the Bohai Bay Basin, but the mechanisms of their genesis and evolution have not been systematically studied. In regard of this, the periods, types and activity characteristics of the faults in this area were analyzed based on the fine stratigraphic interpretation of three-dimensional seismic data and the identification of tectonic styles. Then, the tectonic framework in the key tectonic periods and the formation and evolution process of buried hills were revealed. Finally, the structural characteristics of different zones of buried hills were investigated and the buried hills were classified. And the following research results were obtained. First, there are four stages of tectonic movements inside the buried hills, including Indosinian, early Yanshanian, middle Yanshanian and Himalayan, among which Indosinian and early Yanshanian tectonic movements play a decisive role in controlling the formation and distribution of buried hills. Second, the four stages of tectonic movements formed four sets of complex grid-like fault systems consisting of three groups of faults(i.e. NE, NW and nearly NS faults), which are obviously different from each other in terms of formation stages, natures and activity characteristics. Third, the evolution of this area is divided into four stages, i.e., the formation of material base of buried hills in Paleozoic, the compressive orogeny and the thrust structure development in Late Triassic–Early Jurassic, the intracontinental rift and the formation of buried hill initial patterns in Late Jurassic–Early Cretaceous,and the strike-slip-extension composite transformation and the burial finalization in Cenozoic. Fourth, due to the differences of the manifestations of key tectonic periods, the structural characteristics of the buried hills in this area are obviously zonal, and they are divided into the residual thrust buried hill belt in the west, the inversion tilt buried hill belt in the central area and the complex strike-slip fault block buried hill belt in the east. It is concluded that the Mesozoic and Cenozoic strata in the southwestern Bohai Sea area undergo multicyclic tectonic movements, which result in the diversity of buried hill types and the complexity of the inner fault systems.
引文
[1]翟明国.华北克拉通的形成演化与成矿作用[J].矿床地质,2010,29(1):24-36.Zhai Mingguo.Tectonic evolution and metallogenesis of North China Craton[J].Mineral Deposits,2010,29(1):24-36.
[2]乔秀夫,王彦斌.华北克拉通中元古界底界年龄与盆地性质讨论[J].地质学报,2014,88(9):1623-1637.Qiao Xiufu&Wang Yanbin.Discussions on the lower boundary age of the Mesoproterozoic and basin tectonic evolution of the Mesoproterozoic in North China Craton[J].Acta Geologica Sinica,2014,88(9):1623-1637.
[3]公王斌,胡健民,李振宏,董晓朋,刘洋,刘绍昌.华北克拉通北缘裂谷渣尔泰群LA-ICP-MS碎屑锆石U-Pb测年及地质意义[J].岩石学报,2016,32(7):2151-2165.Gong Wangbin,Hu Jianmin,Li Zhenhong,Dong Xiaopeng,Liu Yang&Liu Shaochang.Detrital zircon U-Pb dating of Zhaertai Group in the north margin rift zone of North China Craton and its implications[J].Acta Petrologica Sinica,2016,32(7):2151-2165.
[4]郝奕玮,骆满生,徐增连,邹亚锐,唐婷婷.华北陆块新元古代-中生代沉积盆地划分及其构造演化[J].地球科学--中国地质大学学报,2014,39(8):1230-1242.Hao Yiwei,Luo Mansheng,Xu Zenglian,Zou Yarui&Tang Tingting.Division of sedimentary basins and its tectonic evolution in North China from Neoproterozoic to Mesozoic[J].Earth Science-Journal of China University of Geosciences,2014,39(8):1230-1242.
[5]赵越,翟明国,陈虹,张拴宏.华北克拉通及相邻造山带古生代-侏罗纪早期大地构造演化[J].中国地质,2017,44(1):44-60.Zhao Yue,Zhai Mingguo,Chen Hong&Zhang Shuanhong.Paleozoic-Early Jurassic tectonic evolution of North China Craton and its adjacent orogenic belts[J].Geology in China,2017,44(1):44-60.
[6]周小进,倪春华,杨帆.华北古生界原型-变形构造演化及其控油气作用[J].石油与天然气地质,2010,31(6):779-794.Zhou Xiaojin,Ni Chunhua&Yang Fan.The Paleozoic prototype basins and their tectonic deformation in North China and their controlling effects upon hydrocarbon accumulation[J].Oil&Gas Geology,2010,31(6):779-794.
[7]李三忠,刘建忠,赵国春,吴福元,韩宗珠,杨中柱.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 Sanzhong,Liu Jianzhong,Zhao Guochun,Wu Fuyuan,Han Zongzhu&Yang Zhongzhu.Key geochronology of Mesozoic deformation in the eastern block of the North China Craton and its constraints on regional tectonics:A case of Jiaodong and Liaodong Peninsula[J].Acta Petrologica Sinica,2004,20(3):633-646.
[8]漆家福,于福生,陆克政,周建勋,王子煜,杨桥.渤海湾地区的中生代盆地构造概论[J].地学前缘,2003,10(增刊1):199-206.Qi Jiafu,Yu Fusheng,Lu Kezheng,Zhou Jianxun,Wang Ziyu&Yang Qiao.Conspectus on Mesozoic basins in Bohai Bay province[J].Earth Science Frontiers,2003,10(S1):199-206.
[9]纪友亮,胡光明,黄建军,吴智平.渤海湾地区中生代地层剥蚀量及中、新生代构造演化研究[J].地质学报,2006,80(3):351-358.Ji Youliang,Hu Guangming,Huang Jianjun&Wu Zhiping.Eroded strata thickness of Mesozoic and evolution of Mesozoic and Cenozoic basins in the Bohai Bay Basin area[J].Acta Geologica Sinica,2006,80(3):351-358.
[10]吴智平,侯旭波,李伟.华北东部地区中生代盆地格局及演化过程探讨[J].大地构造与成矿学,2007,31(4):385-399.Wu Zhiping,Hou Xubo&Li Wei.Discussion on Mesozoic basin patterns and evolution in the eastern North China Block[J].Geotectonica et Metallogenia,2007,31(4):385-399.
[11]李洪颜.华北克拉通原型盆地及岩浆活动时空演化对克拉通破坏的制约[J].中国科学:地球科学,2013,43(9):19-32.Li Hongyan.Destruction of North China Craton:Insights from temporal and spatial evolution of the proto-basins and magmatism[J].Science China:Earth Sciences,2013,43(9):19-32.
[12]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):402-406.Yu Fusheng,Qi Jiafu&Wang Chunying.Tectonic deformation of Indosinian Period in eastern part of North China[J].Journal of China University of Mining&Technology,2002,31(4):402-406.
[13]李勇,钟建华,温志峰,段洪亮,王海侨.印支运动对济阳坳陷构造形态形成演化的影响[J].地质论评,2006,52(3):321-330.Li Yong,Zhong Jianhua,Wen Zhifeng,Duan Hongliang&Wang Haiqiao.Effects of Indosinian movements on tectonic formation and evolution,Jiyang Depression[J].Geological Review,2006,52(3):321-330.
[14]吴梅莲.燕山运动在济阳坳陷的地质表现以及中生界潜山研究[D].武汉:中国地质大学,2007.Wu Meilian.Research on geological manifestation of Yanshan Movement and the Mesozoic buried hills in Jiyang Depression[D].Wuhan:China University of Geosciences,2007.
[15]周立宏,李三忠,刘建忠,高振平.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 Lihong,Li Sanzhong,Liu Jianzhong&Gao Zhenping.The Yanshanian structural style and basin prototypes of the Mesozoic Bohai Bay Basin[J].Progress in Geophysics,2003,18(4):692-699.
[16]薛永安.渤海海域深层天然气勘探的突破与启示[J].天然气工业,2019,39(1):11-20.Xue Yong'an.The breakthrough of the deep-buried gas exploration in the Bohai Sea area and its enlightenment[J].Natural Gas Industry,2019,39(1):11-20.
[17]徐长贵,侯明才,王粤川,陈安清,黄志发,罗小平,等.渤海海域前古近系深层潜山类型及其成因[J].天然气工业,2019,39(1):21-32.Xu Changgui,Hou Mingcai,Wang Yuechuan,Chen Anqing,Huang Zhifa,Luo Xiaoping,et al.Type and genesis of pre-Tertiary deep buried hills in the Bohai Sea area[J].Natural Gas Industry,2019,39(1):21-32.
[18]李三忠,索艳慧,戴黎明,刘丽萍,金宠,刘鑫,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,Liu Liping,Jin Chong,Liu Xin,et al.Development of the Bohai Bay Basin and destruction of the North China Craton[J].Earth Science Frontiers,2010,17(4):64-89.
[19]王金铎.济阳坳陷古潜山中新生代构造演化与油气成藏规律研究[D].青岛:中国海洋大学,2005.Wang Jinduo.Generation and accumulation of hydrocarbon and tectonic evolution of the buried-hill in the Jiyang Depression[D].Qingdao:Ocean University of China,2005.
[20]谭明友,刘福贵,董臣强,冯德永,张桂霞.埕北30潜山构造演化与油气富集规律研究[J].石油地球物理勘探,2002,37(2):134-137.Tan Mingyou,Liu Fugui,Dong Chenqiang,Feng Deyong&Zhang Guixia.Study for evolution of CB30 buried hill structure and rule of oil-gas accumulation[J].Oil Geophysical Prospecting,2002,37(2):134-137.
[21]吴永平,付立新,杨池银,靳久强.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.Wu Yongping,Fu Lixin,Yang Chiyin&Jin Jiuqiang.Effect of Mesozoic tectonic evolution on hydrocarbon accumulation in buried hills in Huanghua Depression[J].Acta Petrolei Sinica,2002,23(2):16-21.
[22]高长海,查明,赵贤正,金凤鸣.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):52-59.Gao Changhai,Zha Ming,Zhao Xianzheng&Jin Fengming.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):52-59.
[23]吕雪莹,蒋有录,刘景东,徐田武.渤海湾盆地杜寨气田深层致密砂岩气成藏机理[J].天然气工业,2018,38(7):34-43.LüXueying,Jiang Youlu,Liu Jingdong&Xu Tianwu.Accumulation mechanism of deep-seated tight sandstone gas reservoirs in the Duzhai Gas Field,Bohai Bay Basin[J].Natural Gas Industry,2018,38(7):34-43.
[24]杜金虎,何海清,赵贤正,张以明,王权,张锐锋,等.渤海湾盆地廊固凹陷杨税务超深超高温奥陶系潜山油气勘探重大突破实践与启示[J].中国石油勘探,2017,22(2):1-12.Du Jinhu,He Haiqing,Zhao Xianzheng,Zhang Yiming,Wang Quan,Zhang Ruifeng,et al.Significant exploration breakthrough in Yangshuiwu ultra-deep and ultra-high temperature Ordovician buried-hill in Langgu Sag,Bohai Bay Basin[J].China Petroleum Exploration,2017,22(2):1-12.
[25]侯贵廷,钱祥麟,蔡东升.渤海湾盆地中、新生代构造演化研究[J].北京大学学报(自然科学版),2001,37(6):845-851.Hou Guiting,Qian Xianglin&Cai Dongsheng.The tectonic evolution of Bohai Basin in Mesozoic and Cenozoic time[J].Acta Scientiarum Naturalium Universitatis Pekinensis,2001,37(6):845-851.
[26]朱光,王薇,顾承串,张帅,刘程.郯庐断裂带晚中生代演化历史及其对华北克拉通破坏过程的指示[J].岩石学报,2016,32(4):935-949.Zhu Guang,Wang Wei,Gu Chengchuan,Zhang Shuai&Liu Cheng.Late Mesozoic evolution history of the Tan-Lu Fault Zone and its indication to the damage process of the North China Craton[J].Acta Petrologica Sinica,2016,32(4):935-949.
[27]徐嘉炜,马国锋.郯庐断裂带研究的十年回顾[J].地质论评,1992,38(4):316-324.Xu Jiawei&Ma Guofeng.Review of ten years(1981-1991)of research on the Tancheng-Lujiang Fault Zone[J].Geological Review,1992,38(4):316-324.
[28]Moore GW.Plate-tectonic evolution of the Circum-Pacific region[C]//1989 AAAS Annual Meeting.AAAS Publication,1988:155.
[2]乔秀夫,王彦斌.华北克拉通中元古界底界年龄与盆地性质讨论[J].地质学报,2014,88(9):1623-1637.Qiao Xiufu&Wang Yanbin.Discussions on the lower boundary age of the Mesoproterozoic and basin tectonic evolution of the Mesoproterozoic in North China Craton[J].Acta Geologica Sinica,2014,88(9):1623-1637.
[3]公王斌,胡健民,李振宏,董晓朋,刘洋,刘绍昌.华北克拉通北缘裂谷渣尔泰群LA-ICP-MS碎屑锆石U-Pb测年及地质意义[J].岩石学报,2016,32(7):2151-2165.Gong Wangbin,Hu Jianmin,Li Zhenhong,Dong Xiaopeng,Liu Yang&Liu Shaochang.Detrital zircon U-Pb dating of Zhaertai Group in the north margin rift zone of North China Craton and its implications[J].Acta Petrologica Sinica,2016,32(7):2151-2165.
[4]郝奕玮,骆满生,徐增连,邹亚锐,唐婷婷.华北陆块新元古代-中生代沉积盆地划分及其构造演化[J].地球科学--中国地质大学学报,2014,39(8):1230-1242.Hao Yiwei,Luo Mansheng,Xu Zenglian,Zou Yarui&Tang Tingting.Division of sedimentary basins and its tectonic evolution in North China from Neoproterozoic to Mesozoic[J].Earth Science-Journal of China University of Geosciences,2014,39(8):1230-1242.
[5]赵越,翟明国,陈虹,张拴宏.华北克拉通及相邻造山带古生代-侏罗纪早期大地构造演化[J].中国地质,2017,44(1):44-60.Zhao Yue,Zhai Mingguo,Chen Hong&Zhang Shuanhong.Paleozoic-Early Jurassic tectonic evolution of North China Craton and its adjacent orogenic belts[J].Geology in China,2017,44(1):44-60.
[6]周小进,倪春华,杨帆.华北古生界原型-变形构造演化及其控油气作用[J].石油与天然气地质,2010,31(6):779-794.Zhou Xiaojin,Ni Chunhua&Yang Fan.The Paleozoic prototype basins and their tectonic deformation in North China and their controlling effects upon hydrocarbon accumulation[J].Oil&Gas Geology,2010,31(6):779-794.
[7]李三忠,刘建忠,赵国春,吴福元,韩宗珠,杨中柱.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 Sanzhong,Liu Jianzhong,Zhao Guochun,Wu Fuyuan,Han Zongzhu&Yang Zhongzhu.Key geochronology of Mesozoic deformation in the eastern block of the North China Craton and its constraints on regional tectonics:A case of Jiaodong and Liaodong Peninsula[J].Acta Petrologica Sinica,2004,20(3):633-646.
[8]漆家福,于福生,陆克政,周建勋,王子煜,杨桥.渤海湾地区的中生代盆地构造概论[J].地学前缘,2003,10(增刊1):199-206.Qi Jiafu,Yu Fusheng,Lu Kezheng,Zhou Jianxun,Wang Ziyu&Yang Qiao.Conspectus on Mesozoic basins in Bohai Bay province[J].Earth Science Frontiers,2003,10(S1):199-206.
[9]纪友亮,胡光明,黄建军,吴智平.渤海湾地区中生代地层剥蚀量及中、新生代构造演化研究[J].地质学报,2006,80(3):351-358.Ji Youliang,Hu Guangming,Huang Jianjun&Wu Zhiping.Eroded strata thickness of Mesozoic and evolution of Mesozoic and Cenozoic basins in the Bohai Bay Basin area[J].Acta Geologica Sinica,2006,80(3):351-358.
[10]吴智平,侯旭波,李伟.华北东部地区中生代盆地格局及演化过程探讨[J].大地构造与成矿学,2007,31(4):385-399.Wu Zhiping,Hou Xubo&Li Wei.Discussion on Mesozoic basin patterns and evolution in the eastern North China Block[J].Geotectonica et Metallogenia,2007,31(4):385-399.
[11]李洪颜.华北克拉通原型盆地及岩浆活动时空演化对克拉通破坏的制约[J].中国科学:地球科学,2013,43(9):19-32.Li Hongyan.Destruction of North China Craton:Insights from temporal and spatial evolution of the proto-basins and magmatism[J].Science China:Earth Sciences,2013,43(9):19-32.
[12]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):402-406.Yu Fusheng,Qi Jiafu&Wang Chunying.Tectonic deformation of Indosinian Period in eastern part of North China[J].Journal of China University of Mining&Technology,2002,31(4):402-406.
[13]李勇,钟建华,温志峰,段洪亮,王海侨.印支运动对济阳坳陷构造形态形成演化的影响[J].地质论评,2006,52(3):321-330.Li Yong,Zhong Jianhua,Wen Zhifeng,Duan Hongliang&Wang Haiqiao.Effects of Indosinian movements on tectonic formation and evolution,Jiyang Depression[J].Geological Review,2006,52(3):321-330.
[14]吴梅莲.燕山运动在济阳坳陷的地质表现以及中生界潜山研究[D].武汉:中国地质大学,2007.Wu Meilian.Research on geological manifestation of Yanshan Movement and the Mesozoic buried hills in Jiyang Depression[D].Wuhan:China University of Geosciences,2007.
[15]周立宏,李三忠,刘建忠,高振平.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 Lihong,Li Sanzhong,Liu Jianzhong&Gao Zhenping.The Yanshanian structural style and basin prototypes of the Mesozoic Bohai Bay Basin[J].Progress in Geophysics,2003,18(4):692-699.
[16]薛永安.渤海海域深层天然气勘探的突破与启示[J].天然气工业,2019,39(1):11-20.Xue Yong'an.The breakthrough of the deep-buried gas exploration in the Bohai Sea area and its enlightenment[J].Natural Gas Industry,2019,39(1):11-20.
[17]徐长贵,侯明才,王粤川,陈安清,黄志发,罗小平,等.渤海海域前古近系深层潜山类型及其成因[J].天然气工业,2019,39(1):21-32.Xu Changgui,Hou Mingcai,Wang Yuechuan,Chen Anqing,Huang Zhifa,Luo Xiaoping,et al.Type and genesis of pre-Tertiary deep buried hills in the Bohai Sea area[J].Natural Gas Industry,2019,39(1):21-32.
[18]李三忠,索艳慧,戴黎明,刘丽萍,金宠,刘鑫,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,Liu Liping,Jin Chong,Liu Xin,et al.Development of the Bohai Bay Basin and destruction of the North China Craton[J].Earth Science Frontiers,2010,17(4):64-89.
[19]王金铎.济阳坳陷古潜山中新生代构造演化与油气成藏规律研究[D].青岛:中国海洋大学,2005.Wang Jinduo.Generation and accumulation of hydrocarbon and tectonic evolution of the buried-hill in the Jiyang Depression[D].Qingdao:Ocean University of China,2005.
[20]谭明友,刘福贵,董臣强,冯德永,张桂霞.埕北30潜山构造演化与油气富集规律研究[J].石油地球物理勘探,2002,37(2):134-137.Tan Mingyou,Liu Fugui,Dong Chenqiang,Feng Deyong&Zhang Guixia.Study for evolution of CB30 buried hill structure and rule of oil-gas accumulation[J].Oil Geophysical Prospecting,2002,37(2):134-137.
[21]吴永平,付立新,杨池银,靳久强.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.Wu Yongping,Fu Lixin,Yang Chiyin&Jin Jiuqiang.Effect of Mesozoic tectonic evolution on hydrocarbon accumulation in buried hills in Huanghua Depression[J].Acta Petrolei Sinica,2002,23(2):16-21.
[22]高长海,查明,赵贤正,金凤鸣.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):52-59.Gao Changhai,Zha Ming,Zhao Xianzheng&Jin Fengming.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):52-59.
[23]吕雪莹,蒋有录,刘景东,徐田武.渤海湾盆地杜寨气田深层致密砂岩气成藏机理[J].天然气工业,2018,38(7):34-43.LüXueying,Jiang Youlu,Liu Jingdong&Xu Tianwu.Accumulation mechanism of deep-seated tight sandstone gas reservoirs in the Duzhai Gas Field,Bohai Bay Basin[J].Natural Gas Industry,2018,38(7):34-43.
[24]杜金虎,何海清,赵贤正,张以明,王权,张锐锋,等.渤海湾盆地廊固凹陷杨税务超深超高温奥陶系潜山油气勘探重大突破实践与启示[J].中国石油勘探,2017,22(2):1-12.Du Jinhu,He Haiqing,Zhao Xianzheng,Zhang Yiming,Wang Quan,Zhang Ruifeng,et al.Significant exploration breakthrough in Yangshuiwu ultra-deep and ultra-high temperature Ordovician buried-hill in Langgu Sag,Bohai Bay Basin[J].China Petroleum Exploration,2017,22(2):1-12.
[25]侯贵廷,钱祥麟,蔡东升.渤海湾盆地中、新生代构造演化研究[J].北京大学学报(自然科学版),2001,37(6):845-851.Hou Guiting,Qian Xianglin&Cai Dongsheng.The tectonic evolution of Bohai Basin in Mesozoic and Cenozoic time[J].Acta Scientiarum Naturalium Universitatis Pekinensis,2001,37(6):845-851.
[26]朱光,王薇,顾承串,张帅,刘程.郯庐断裂带晚中生代演化历史及其对华北克拉通破坏过程的指示[J].岩石学报,2016,32(4):935-949.Zhu Guang,Wang Wei,Gu Chengchuan,Zhang Shuai&Liu Cheng.Late Mesozoic evolution history of the Tan-Lu Fault Zone and its indication to the damage process of the North China Craton[J].Acta Petrologica Sinica,2016,32(4):935-949.
[27]徐嘉炜,马国锋.郯庐断裂带研究的十年回顾[J].地质论评,1992,38(4):316-324.Xu Jiawei&Ma Guofeng.Review of ten years(1981-1991)of research on the Tancheng-Lujiang Fault Zone[J].Geological Review,1992,38(4):316-324.
[28]Moore GW.Plate-tectonic evolution of the Circum-Pacific region[C]//1989 AAAS Annual Meeting.AAAS Publication,1988:155.
© 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 |