渤海湾盆地冀中坳陷中区中新生代复合伸展构造
|
摘要
通过对大量地震剖面的重新解释,并结合盆地的钻探资料及前人研究成果,揭示了冀中坳陷中区中新生代以来先后经历了:①燕山中晚期(J3-K1)与阜平变质核杂岩形成有关的热力伸展,变质核杂岩拱升隆起导致侧向伸展,太行山东缘拆离断层发育并在其下降盘形成同期断陷盆地(保定凹陷);②古近纪(E)区域应力伸展,太行山东缘断裂及其下降盘的保定凹陷具有明显的继承性,并有"早盛早衰"的特点。而中区东部边缘断裂及其控制的沉积洼槽主要发育于该阶段,断裂强烈活动时间相对晚,但持续时间铰长;⑧古、新近纪之间(N／E)重力伸展,区域不均衡隆升导致饶阳凹陷南部发生大型重力滑覆构造,其运动轨迹类似昆虫前行时的"褶曲蠕动",与经典的重力滑动构造模式有所不同。三期不同性质、不同类型的伸展作用有机相联,彼此影响,并进一步探讨了各类伸展构造的个性特征、形成演化及其盆山耦合的响应关系。
Based on the interpretation of the seismic profiles in the middle Jizhong depression, it is pointed out that the area underwent three types of extension since the mid-Mesozoic, that is, heat doming extension, stress extension and gravity extension. The heat doming extension related with the Fuping nuclear complex took place in the Taihang Mountains in the middle-late Mesozoic. Doming of the nuclear complex lead to lateral extension and detachment faults were developed on the east margin of the Taihangshan Mountains to form a contemporaneous down-faulted basin (Baoding depression) in the foot wall. It is well known that the Bohai Bay Basin came into a stress extension stage in the Eogene, during which the detachment fault and normal fault are two types of growing faults. The former dips gently in shallow layers, but steeply in deep layers of the crust and becomes a horizontal ductile shear zone at the bottom, expressing strongly horizontal extension, whereas the latter has a small extension. A large-scale detachment structure was distinguished in the south area of the Raoyang depression. It is bounded by the Cangxi fault in the east, the Lixian slop in the west, the north Liulu fault in the north and the Hengshui fault in the south. The area is near 2000 km2. This took place due to gravity gliding after the unbalanced uplifting of the Cangxian bulge at the end of the Eogene. This structure is characterized by clear detachment faults, two different deformation systems, as well as the front edge and back edge. The gliding track in the area is like a crawl tract of insects. This is a new gravity gliding model. The three types of extensional structures are connected to each other, influence each other, and there are clear coupling relationships between basins and mountains.
Based on the interpretation of the seismic profiles in the middle Jizhong depression, it is pointed out that the area underwent three types of extension since the mid-Mesozoic, that is, heat doming extension, stress extension and gravity extension. The heat doming extension related with the Fuping nuclear complex took place in the Taihang Mountains in the middle-late Mesozoic. Doming of the nuclear complex lead to lateral extension and detachment faults were developed on the east margin of the Taihangshan Mountains to form a contemporaneous down-faulted basin (Baoding depression) in the foot wall. It is well known that the Bohai Bay Basin came into a stress extension stage in the Eogene, during which the detachment fault and normal fault are two types of growing faults. The former dips gently in shallow layers, but steeply in deep layers of the crust and becomes a horizontal ductile shear zone at the bottom, expressing strongly horizontal extension, whereas the latter has a small extension. A large-scale detachment structure was distinguished in the south area of the Raoyang depression. It is bounded by the Cangxi fault in the east, the Lixian slop in the west, the north Liulu fault in the north and the Hengshui fault in the south. The area is near 2000 km2. This took place due to gravity gliding after the unbalanced uplifting of the Cangxian bulge at the end of the Eogene. This structure is characterized by clear detachment faults, two different deformation systems, as well as the front edge and back edge. The gliding track in the area is like a crawl tract of insects. This is a new gravity gliding model. The three types of extensional structures are connected to each other, influence each other, and there are clear coupling relationships between basins and mountains.
引文
董树文,吴锡浩,吴珍汉,等.2000.论东亚大陆的构造翘变.地质 论评,46(1):8-13.
何海清,王兆云,韩品龙.1998.华北地区构造演化对渤海湾油气 形成和分布的控制.地质学报,72(4):313-321.
刘池阳.1990.渤海湾盆地的裂陷伸展与断块翘倾.见:赵重远,刘 池阳编著,华北克拉通沉积盆地形成及其油气赋存.西安:西 北大学出版社,30-42.
刘和甫,梁慧社,李晓清,等.2000.中国东部中新生代裂陷盆地与 伸展山岭的耦合机制.地学前缘,7(4):477-486.
罗照华,邓晋福,赵国春,等.1997.太行造山带岩浆活动及造山过 程反演.地球科学,22(3):279-284.
马杏垣,刘和甫,王维襄,等.1983.中国东部中、新生代裂陷作用 和伸展构造.地质学报,57(1):22-32.
马杏垣.1989.重力作用与构造运动.北京:地震出版社,10-120.
牛树银,董国润,许传诗,1995.论太行山构造岩浆带的岩浆来源 及成因.地质论评,41(4):301-310.
牛树银.1994.太行山阜平、赞皇隆起是中新生代变质核杂岩.地质 科技情报,13(2):15-16.
任纪舜,陈延愚,牛宝贵,等.1990.中国东部大陆岩石圈的构造演 化与成矿.北京:科学出版社,1-205.
任建业,胡祥云,张俊霞.1998.中国大陆东部晚中生代构造活化 及其演化过程.大地构造及成矿学,22(2):89-96.
任战利.1999.中国北方沉积盆地构造热演化史研究.北京:石油工 业出版社,20-80.
舒良树,孙岩,王德滋,等.1998。华南武功山中生代伸展构造.中 国科学(D辑),28(5):431-438.
宋鸿林.1996.北京房山变质核杂岩的基本特征及其成因探讨.现 代地质,2(10):149-158.
孙冬胜.2001.冀中坳陷中区中新生代复合伸展构造.西北大学博 士学位论文,18-79.
陶明华,王开发,郑国光,等.2000.冀中坳陷早第三纪孢粉组合及 地质时代讨论,微体古生物学报,18(3):274-292.
陶明华,邹伟宏.2000.中国早第三纪孢粉组合序列及两条主要地 层界线的讨论.见:朱宗浩,郑国光,赵传本,主编.中国含油 气盆地孢粉论文集.北京:石油工业出版社,62-80.
汪洋,邓晋福.2002.冀晋辽地区燕山期强过铝质侵入岩岩石化学 特征及其动力学意义.地质通报,21(4-5);270-276.
徐杰,高战武,孙建宝,等.2001.区域伸展体制下盆-山耦合关系 的探讨--以渤海湾盆地和太行山为例.地质学报,75(2): 165-174.
许文良,王冬艳,王嗣敏.2000.中国东部中新生代火山作用pTtc 模型与岩石圈演化.长春科技大学学报,30(4):229-335.
张家声,徐杰,万景林,等.2002.太行山山前中-新生代伸展拆离 构造和年代学.地质通报,21(4-5):207-210.
张旗,钱青,王二七,等.2001a.燕山中晚期的中国东部高原:埃达 克岩的启示.地质科学,36(2):248-255.
张旗,赵太平,王焰,等.2001b.中国东部燕山期岩浆活动的几个 问题.岩石矿物学杂志,20(3):273-280.
赵越,杨振宇,马醒华.1994.东亚大陆构造发展的重要转折.地质 科学,29(2):105-119.
朱志澄.1987.伸展构造和拆离断层.地质科技情报,6(1):19- 22.
朱志澄.1994.变质核杂岩和伸展构造研究述评.地质科技情报, 13(3):1-9.
Dong S W, Wu X H, Wu Z H, et. al. 2000. Discussion on wrap and changing in eastern continent of Asia. Geological Review, 46(1) : 8-13(in Chinese with English abstract).
He H Q, Wang Z Y, Han P L. 1998. The controlling of the tectonic evolution in northern China on the formation and distribution of oil and gas in Bohai Bay area. Acta Geologica Sinica, 72 (4) : 313-321 (in Chinese with English abstract).
Liu C Y. 1990. The taphrogeny-extension and the tilting of fault blocks in Bohaiwan basin. See Zhao Z Y, Liu C Y, The formation and evolution of the sedimentary basins and their hydrocarbon occurrence in the north China craton. Xian: Northwest University Press,30-42.
Liu H F,Liang H S, LI X Q,et al. 2000. The coupling mechanisms of Mesozoic-Cenozoic rift basins and extensional mountain system in eastern China. Earth Science Frontiers, 7 (4): 477 - 486 (in Chinese with English abstract).
Luo Z H, Deng J F, Zhao G C, et al. 1997. Characteristics of magmatic activities and orogenic process of Taihang Mountains intraplate orogen. Earth Science (Journal of China University of Geosciences), 22 (3): 279 - 284 (in Chinese with English abstract).
Ma X Y, Liu H F, Wang W X,et al. 1983. Mesozoic-Cenozoic rift and extensional tectonic in Eastern China. Acta Geologica Sinica, 57(1) :22-32(in Chinese).
Ma X Y. 1989. Gravity action and tectonic movement. Beijing: Seismological Press,10-120(in Chinese).
Morely C K. 1999. Pattern of displacement analog large normal faults: Implications for basin evolution and fault propagation, based on example from east Africa. AAPG, 83(4) :613-634.
Muraoka H, Kamata H. 1983. Displacement distribution along minor fault traces. J. Struct. Geol. , 5: 483-495.
Niu S Y, Dong G R, Xu C S. 1995. The discussion on organic in Taihang Mountains tectonic and organic zone. Geological Review, 41(4):301-310(in Chinese with English abstract).
Niu S Y. 1994. Fuping and Zanhuang uplift in Taihang Mountains are Meso-Cenozoic metamorphic core complex. Geological Science and Technology Information, 13(2) :15-16(in Chinese with English abstract).
Ren J S, Chen Y Y, Niu B G, et al. 1990. The tectonic evolution and mineral forming of continental lithosphere in the eastern China. Beijing: Science Press, l-205(in Chinese).
Ren J Y, Hu X Y, Zhang J X. 1998. The late Mesozoic tectonic activation in the eastern Chinese continent and its evolution process. Geotectonic et Metallogenia, 22(2): 89- 96 (in Chinese with English abstract).
Ren Z L. 1999. The evolution of tectonic and thermal in the northern basins of China. Beijing: Petroleum Industry Press, 20 - 80(in Chinese).
Shu L S, Sun Y, Wang D Z, et al. 1998. Mesonic extensional tectonic in Wugong Mountains of Southern China. Science in China (Series D),28(5) :431-438(in Chinese).
Song H L. 1996. Characteristics of Fanshan metamorphic core complex, Beijing and discussion about its origin. Geoscience (Journal of Graduate School, China University of Geosciences), 10(2):149-158(in Chinese with English abstract).
Sun D S. 2001. The study on complex extensional structures in themiddle area of Jizhong Depression of Bohai Bay Basin, Doctor paper of Northwest University, 18- 79(in Chinese with English abstract).
Tao M H, Wang K F, Zheng G G. et al. 2001. Early Tertiary sporopollen assemblages from Jizhong depression and their stratigraphic implication. Acta Micropalaeontologica Sinica, 18 (3) :274-292(in Chinese with English abstract).
Tao M H, Zou W H. 2000. The Plaeogene sporopollen assemblage series in China and discussion on two important stratigraphic boundary. See Zhu Z h, Zheng G G, Zhao C B, Symposium on Palynology of petroliferous basins in China. Beijng: Petroleum Industry Press, 62-80.
Wang Y, Deng J F. 2002. Petrochemical characteristics and geodynamic significance of Yanshanian strongly peraluminous intrusive rocks in the Hebei-Shanxi-Liaoning area. Geological Bulletin of China, 21 (4-5) : 270 -276 (in Chinese with English abstract).
Xu J, Gao Z W, Sun J B, et al. 2001. A preliminary study of coupling relation between basin and mountain in extensional environments - A case study of the Bohai Bay Basin and Taihang Mountains, Acta Geologica Sinica,75(2) : 165- 174(in Chinese with English abstract).
Xu W L, Wang D Y, Wang S M. 2000. pTtc model of Mesozoic and Cenozoic volcanisms and lithosphere evolution in eastern China. Journal of Changchun University of Science and Technology, 30(4) : 229-335(in Chinese with English abstract).
Zhang J S, Xu J, Wang J L, et al. 2002. Meso-Cenozonic detachmentzones in the front of the Taihang Mountains and their fission-trackages, Geological Bullet in of China, 21 (4 - 5): 207 - 210 (inChinese with English abstract)
Zhang Q, Qing Q, Wang E C, et al. 2001. An east chain plateau inmid-late Yanshanian period.. Implication from Adakites. ChineseJournal of Geology, 36(2):248-255(in Chinese with Englishabstract).
Zhang Q, Zhao T P, Wang Y, et al. 2001. A Discussion on theYanshanian Magmatism in east China, Acta Petrologica etMineralogica, 20 (3): 273 - 280 (in Chinese with Englishabstract).
Zhao Y, Yang Z N, Ma X H. 1994. Geotectonic transition frompaleo-Asian system and plaeo-Tethyan system to plaeo-Pacificactive continental margin in eastern Asia, Scientia GeologicaSinica, 29(2) :105-119(in Chinese with English abstract).
Zhao Z Y, 1984. The tectonic pattern and evolution in Bohai BayBasin. Acta Petrolei Sinica,5(1): 1 - 8(in Chinese with Englishabstract).
Zhu Z C. 1987. Extensional tectonic and detachment fault. GeologicalScience and Technology Information, 6(1) :19-22(in Chinese).
Zhu Z C. 1994. Review on metamorphic core complex and extensionaltectonic. Geological Science and Technology Information, 13(3):1 - 9(in Chinese with English abstract).
何海清,王兆云,韩品龙.1998.华北地区构造演化对渤海湾油气 形成和分布的控制.地质学报,72(4):313-321.
刘池阳.1990.渤海湾盆地的裂陷伸展与断块翘倾.见:赵重远,刘 池阳编著,华北克拉通沉积盆地形成及其油气赋存.西安:西 北大学出版社,30-42.
刘和甫,梁慧社,李晓清,等.2000.中国东部中新生代裂陷盆地与 伸展山岭的耦合机制.地学前缘,7(4):477-486.
罗照华,邓晋福,赵国春,等.1997.太行造山带岩浆活动及造山过 程反演.地球科学,22(3):279-284.
马杏垣,刘和甫,王维襄,等.1983.中国东部中、新生代裂陷作用 和伸展构造.地质学报,57(1):22-32.
马杏垣.1989.重力作用与构造运动.北京:地震出版社,10-120.
牛树银,董国润,许传诗,1995.论太行山构造岩浆带的岩浆来源 及成因.地质论评,41(4):301-310.
牛树银.1994.太行山阜平、赞皇隆起是中新生代变质核杂岩.地质 科技情报,13(2):15-16.
任纪舜,陈延愚,牛宝贵,等.1990.中国东部大陆岩石圈的构造演 化与成矿.北京:科学出版社,1-205.
任建业,胡祥云,张俊霞.1998.中国大陆东部晚中生代构造活化 及其演化过程.大地构造及成矿学,22(2):89-96.
任战利.1999.中国北方沉积盆地构造热演化史研究.北京:石油工 业出版社,20-80.
舒良树,孙岩,王德滋,等.1998。华南武功山中生代伸展构造.中 国科学(D辑),28(5):431-438.
宋鸿林.1996.北京房山变质核杂岩的基本特征及其成因探讨.现 代地质,2(10):149-158.
孙冬胜.2001.冀中坳陷中区中新生代复合伸展构造.西北大学博 士学位论文,18-79.
陶明华,王开发,郑国光,等.2000.冀中坳陷早第三纪孢粉组合及 地质时代讨论,微体古生物学报,18(3):274-292.
陶明华,邹伟宏.2000.中国早第三纪孢粉组合序列及两条主要地 层界线的讨论.见:朱宗浩,郑国光,赵传本,主编.中国含油 气盆地孢粉论文集.北京:石油工业出版社,62-80.
汪洋,邓晋福.2002.冀晋辽地区燕山期强过铝质侵入岩岩石化学 特征及其动力学意义.地质通报,21(4-5);270-276.
徐杰,高战武,孙建宝,等.2001.区域伸展体制下盆-山耦合关系 的探讨--以渤海湾盆地和太行山为例.地质学报,75(2): 165-174.
许文良,王冬艳,王嗣敏.2000.中国东部中新生代火山作用pTtc 模型与岩石圈演化.长春科技大学学报,30(4):229-335.
张家声,徐杰,万景林,等.2002.太行山山前中-新生代伸展拆离 构造和年代学.地质通报,21(4-5):207-210.
张旗,钱青,王二七,等.2001a.燕山中晚期的中国东部高原:埃达 克岩的启示.地质科学,36(2):248-255.
张旗,赵太平,王焰,等.2001b.中国东部燕山期岩浆活动的几个 问题.岩石矿物学杂志,20(3):273-280.
赵越,杨振宇,马醒华.1994.东亚大陆构造发展的重要转折.地质 科学,29(2):105-119.
朱志澄.1987.伸展构造和拆离断层.地质科技情报,6(1):19- 22.
朱志澄.1994.变质核杂岩和伸展构造研究述评.地质科技情报, 13(3):1-9.
Dong S W, Wu X H, Wu Z H, et. al. 2000. Discussion on wrap and changing in eastern continent of Asia. Geological Review, 46(1) : 8-13(in Chinese with English abstract).
He H Q, Wang Z Y, Han P L. 1998. The controlling of the tectonic evolution in northern China on the formation and distribution of oil and gas in Bohai Bay area. Acta Geologica Sinica, 72 (4) : 313-321 (in Chinese with English abstract).
Liu C Y. 1990. The taphrogeny-extension and the tilting of fault blocks in Bohaiwan basin. See Zhao Z Y, Liu C Y, The formation and evolution of the sedimentary basins and their hydrocarbon occurrence in the north China craton. Xian: Northwest University Press,30-42.
Liu H F,Liang H S, LI X Q,et al. 2000. The coupling mechanisms of Mesozoic-Cenozoic rift basins and extensional mountain system in eastern China. Earth Science Frontiers, 7 (4): 477 - 486 (in Chinese with English abstract).
Luo Z H, Deng J F, Zhao G C, et al. 1997. Characteristics of magmatic activities and orogenic process of Taihang Mountains intraplate orogen. Earth Science (Journal of China University of Geosciences), 22 (3): 279 - 284 (in Chinese with English abstract).
Ma X Y, Liu H F, Wang W X,et al. 1983. Mesozoic-Cenozoic rift and extensional tectonic in Eastern China. Acta Geologica Sinica, 57(1) :22-32(in Chinese).
Ma X Y. 1989. Gravity action and tectonic movement. Beijing: Seismological Press,10-120(in Chinese).
Morely C K. 1999. Pattern of displacement analog large normal faults: Implications for basin evolution and fault propagation, based on example from east Africa. AAPG, 83(4) :613-634.
Muraoka H, Kamata H. 1983. Displacement distribution along minor fault traces. J. Struct. Geol. , 5: 483-495.
Niu S Y, Dong G R, Xu C S. 1995. The discussion on organic in Taihang Mountains tectonic and organic zone. Geological Review, 41(4):301-310(in Chinese with English abstract).
Niu S Y. 1994. Fuping and Zanhuang uplift in Taihang Mountains are Meso-Cenozoic metamorphic core complex. Geological Science and Technology Information, 13(2) :15-16(in Chinese with English abstract).
Ren J S, Chen Y Y, Niu B G, et al. 1990. The tectonic evolution and mineral forming of continental lithosphere in the eastern China. Beijing: Science Press, l-205(in Chinese).
Ren J Y, Hu X Y, Zhang J X. 1998. The late Mesozoic tectonic activation in the eastern Chinese continent and its evolution process. Geotectonic et Metallogenia, 22(2): 89- 96 (in Chinese with English abstract).
Ren Z L. 1999. The evolution of tectonic and thermal in the northern basins of China. Beijing: Petroleum Industry Press, 20 - 80(in Chinese).
Shu L S, Sun Y, Wang D Z, et al. 1998. Mesonic extensional tectonic in Wugong Mountains of Southern China. Science in China (Series D),28(5) :431-438(in Chinese).
Song H L. 1996. Characteristics of Fanshan metamorphic core complex, Beijing and discussion about its origin. Geoscience (Journal of Graduate School, China University of Geosciences), 10(2):149-158(in Chinese with English abstract).
Sun D S. 2001. The study on complex extensional structures in themiddle area of Jizhong Depression of Bohai Bay Basin, Doctor paper of Northwest University, 18- 79(in Chinese with English abstract).
Tao M H, Wang K F, Zheng G G. et al. 2001. Early Tertiary sporopollen assemblages from Jizhong depression and their stratigraphic implication. Acta Micropalaeontologica Sinica, 18 (3) :274-292(in Chinese with English abstract).
Tao M H, Zou W H. 2000. The Plaeogene sporopollen assemblage series in China and discussion on two important stratigraphic boundary. See Zhu Z h, Zheng G G, Zhao C B, Symposium on Palynology of petroliferous basins in China. Beijng: Petroleum Industry Press, 62-80.
Wang Y, Deng J F. 2002. Petrochemical characteristics and geodynamic significance of Yanshanian strongly peraluminous intrusive rocks in the Hebei-Shanxi-Liaoning area. Geological Bulletin of China, 21 (4-5) : 270 -276 (in Chinese with English abstract).
Xu J, Gao Z W, Sun J B, et al. 2001. A preliminary study of coupling relation between basin and mountain in extensional environments - A case study of the Bohai Bay Basin and Taihang Mountains, Acta Geologica Sinica,75(2) : 165- 174(in Chinese with English abstract).
Xu W L, Wang D Y, Wang S M. 2000. pTtc model of Mesozoic and Cenozoic volcanisms and lithosphere evolution in eastern China. Journal of Changchun University of Science and Technology, 30(4) : 229-335(in Chinese with English abstract).
Zhang J S, Xu J, Wang J L, et al. 2002. Meso-Cenozonic detachmentzones in the front of the Taihang Mountains and their fission-trackages, Geological Bullet in of China, 21 (4 - 5): 207 - 210 (inChinese with English abstract)
Zhang Q, Qing Q, Wang E C, et al. 2001. An east chain plateau inmid-late Yanshanian period.. Implication from Adakites. ChineseJournal of Geology, 36(2):248-255(in Chinese with Englishabstract).
Zhang Q, Zhao T P, Wang Y, et al. 2001. A Discussion on theYanshanian Magmatism in east China, Acta Petrologica etMineralogica, 20 (3): 273 - 280 (in Chinese with Englishabstract).
Zhao Y, Yang Z N, Ma X H. 1994. Geotectonic transition frompaleo-Asian system and plaeo-Tethyan system to plaeo-Pacificactive continental margin in eastern Asia, Scientia GeologicaSinica, 29(2) :105-119(in Chinese with English abstract).
Zhao Z Y, 1984. The tectonic pattern and evolution in Bohai BayBasin. Acta Petrolei Sinica,5(1): 1 - 8(in Chinese with Englishabstract).
Zhu Z C. 1987. Extensional tectonic and detachment fault. GeologicalScience and Technology Information, 6(1) :19-22(in Chinese).
Zhu Z C. 1994. Review on metamorphic core complex and extensionaltectonic. Geological Science and Technology Information, 13(3):1 - 9(in Chinese with English abstract).
版权所有：© 2023 中国地质图书馆 中国地质调查局地学文献中心