渤海海域西南部前新生代反转构造特征及成因机制
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摘要
渤海西南海域前新生代发育多种类型的反转构造,不同类型的反转构造对研究区中生代构造演化具有重要的指示意义。基于钻井及三维地震资料,总结了研究区前中生代反转构造特征,并探讨了其成因机制。结果表明:(1)研究区发育正、负两期反转,其中负反转构造以反转断层为主,根据反转断层在新生代是否活动,将其进一步划分为长期活动型反转断层与短期活动型反转断层;(2)受控于早期断层的规模及刚性基岩的差异支撑作用,不同的反转断层具有差异的活动时间及其走向;正反转构造则以反转背斜为主;(3)两期反转构造是对华北板块燕山运动的有效记录,其中早期负反转构造记录了燕山运动Ⅰ幕、Ⅱ幕造山运动后岩石圈的裂解过程,而正反转构造则是燕山运动Ⅲ幕太平洋板块NW向俯冲的持续响应。
Various types of inversion structures developed in the southwest Bohai sea in the pre-Cenozoic,which has great significance for the tectonic evolution of Mesozoic.Based on the drilling and 3D seismic data,the characteristic of the inversion structure in the study area is summarized and the genetic mechanism is discussed.The result shows that(1)two phases of inversion tectonics have been identified which are negative inversion structure and positive reversal anticline.The negative inversion structures are mainly negative inversion fault,which can be devided into long-term active inversion fault and short-term active inversion fault according to the activity of the fault in Cenozoic,(2)the scale of the early faults and the support of the rigid basement control the difference of the activity and the trend of the inversion fault,and the the reverse anticline is the dominant positive reverse structure,(3)The two-phase inversion is a good record of the Yanshan Movement in the research area.Negative inversion structure recorded the process of the post-tectonic curtain lithosphere collapse during theⅠ and Ⅱ phase of Yanshan Movement,and the positive inversion structure is the sustained response of the NW-trending subduction of Pacific plate to the curtain during theⅢ phase of Yanshan Movement.
Various types of inversion structures developed in the southwest Bohai sea in the pre-Cenozoic,which has great significance for the tectonic evolution of Mesozoic.Based on the drilling and 3D seismic data,the characteristic of the inversion structure in the study area is summarized and the genetic mechanism is discussed.The result shows that(1)two phases of inversion tectonics have been identified which are negative inversion structure and positive reversal anticline.The negative inversion structures are mainly negative inversion fault,which can be devided into long-term active inversion fault and short-term active inversion fault according to the activity of the fault in Cenozoic,(2)the scale of the early faults and the support of the rigid basement control the difference of the activity and the trend of the inversion fault,and the the reverse anticline is the dominant positive reverse structure,(3)The two-phase inversion is a good record of the Yanshan Movement in the research area.Negative inversion structure recorded the process of the post-tectonic curtain lithosphere collapse during theⅠ and Ⅱ phase of Yanshan Movement,and the positive inversion structure is the sustained response of the NW-trending subduction of Pacific plate to the curtain during theⅢ phase of Yanshan Movement.
引文
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Hayward A B,Graham R H.1989.Some geometric characteristics of inversion.In:Cooper MA and Williams GD(eds.).Inversion Tectonics.Geological Society,London,Special Publication,44:17~39.
Hou GT,Qian X L,Cai D S.2001.The Tectonic Evolution of Bohai Basin in Mesozoic and Cenozoic Time.Acta Scicentiarum Naturalum Universitis Pekinesis,37(6):845~851.
Hou X B,Wu Z P,Li W.2010.Development characteristics of Mesozoic negative inversion structures in Jiyang depression.Journal of China University of Petroleum(Edition of Natural Science),34(1):18~24.
Hou G T,Qian X L,Song X M.1998.The Origin of the Bohai Bay Basin.Acta Scicentiarum Naturalum Universitis Pekinesis.
Iaffa D N,Sàbat F,Bello D,Ferrer O,Mon R,Gutierrez A A.2011.Tectonic inversion in a segmented foreland basin from extensional to piggy back settings:The Tucumàn basin inNWArgentina.Journal of Asian Earth Sciences,31:457~474.
Jiang H,Wang H,Xiao J,Lin Z L,Lv X J,Cai J.2008.Tectonic inversion and its relationship with hydrocarbon accumulation in Zhu-3Depression of Pearl River Mouth Basin.Acta Petrolei Sinica,29(3):372~378.
Lei C,Ren J Y,Wu M L,Qi P L,Hu D S.2008.The Quantificational analysis of development and evolvement of Guxi negative inversion fault and its significance in petroleum geology in Jiyang depression.Geotectonica Et Metallogenia,32(4):462~469.
Li S Z,Suo Y H,Dai L M,Liu L P,Jin C,Liu X,Hao T Y,Zhou L H,Liu B H,Zhou J T,Jiao Q.2010.Development of the Bohai Bay Basin and destruction of the North China Craton.Earth Science Frontiers,17(4):64~89.
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.
Liu Z L,Xia B.2006.Prelimnary restores of the mesozoic original basin and its main control factors in jiyang sag.Natural Gas Geoscience 17(1),60~63.
Qi J F,Yang Q,Lu K Z,Zhou J X,Wang Z Y.2004.Geologic map of sub-outcrop and its implied informationof tectogenesis in Bohai Bay basin province.Earth Science Frontiers,11(3)299~306.
Qi J F,Yu F S,Lu K Z,Zhou J X,Wang Z Y,Yang Q.2003.Conspectus on Mesozoic basins in Bohai bay province.Earth Science Frontiers,10(S1):199~207.
Qiang K S,Lv X X,Zhou X H,Xu C G,Tu D F,Lan X D.2013.Relationship between JX1-1 Inversion Tectonics and Hydrocarbon Accumulation of the Northern Offshore Bohai Bay Basin.Natural Gas Geoscience,24(2):329~334.
Sibson R H.1995.Selective fault reactivation during basin inversion:Potential for fluid redistribution through fault-value action.In Buchanan JV and Buchanan PG(eds.).Basin Inversion.Geological Society,London,Special Publication,88:3~19.
Thomas D W,Coward M.P.1996.Mesozoic regional tectonics and South Viking Graben formation:evidence for localized thinskinned detachments during rift development and inversion.Marine and Petroleum Geology,13(20):149~177.
Hassan W,Nadi A,2015.Impact of inversion tectonics on hydrocarbon entrapment in the Baggara Basin,Western Sudan.Marine and Petroleum Geology,68:492~497.
Hassan W,Farwa A G,Awad M Z.2017.Inversion tectonics in Central Africa Rift System:Evidence from the Heglig Field.Marine and Petroleum Geology,80:293~306.
Wang G C.1998.Relationship of Tanlu fault to the inversion and flower structures in Bohai bay.China offshore oil and gas,12(5):289~295.
Wang Q,Li S Z,Guo L L,Suo Y H,Dai L M.2017.Analogue modeling and mechanism of tectonic inversion of the Xihu Sag,East China Sea Shelf Basin.Journal of Asian Earth Sciences,139:129~141.
Wang Z C,Liu H F,Duan Z F,Wang H Y.1998.Analysis of Meso-Cenozoic tectonic inversion of Huanghua depression.Earth Science,23(3):289~293.
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 11,358~399.(in Chinese).
Xiao D S.2012.Lower Paleozoic Burial Stratigraphy and ReservoirCap Assemblages in Nanpu Sag,Bohai Bay Basin.Natural Gas Geoscience,23(1):68~73.
Yang K J,Qi J F,Yu Y X,Ma B J,Ping Y Q,Xu C G.2016.The inversion structures within Liaozhong depression and its responds to the strike-slip activities of Tan-Lu fault zone.Acta petrologica Sinica,32(4):1182~1196.
Ye T,Wei A J,Peng J S,Gao K S,Deng H,Lu F T,Guo Y,Ren Y P.2018.Characteristics and reservoir-forming differences of volcanic lithofacies in Yixian formation of Cretaceous in Bohai Bay area.Journal of China University of Mining&Technolog,47(5):1083~1094.
Ye T,Wei A J,Zhu C R,Wang Y C,Gao K S,Zeng J C.2016.Characteristic and Petroleum Exploration of Mesozoic Basement“Destructive Volcanic Edifices”in Bohai Bay Area.Acta Petrolei Sinica,37(11):1370~1381.
Yu Y X,Zhou X H,Xu C G,Wei G,Lv D Y.2017.Differential Structural Deformation of Tan-Lu Fault Zone and Hydrocarbon Accumulation in Offshore Bohai Bay Basin,Geological Review,63(supp.):81~82.
Yuan J W,Jia D,Wang M M,Li Y Q,Shen S X.2015.Structural Characteristics of Negative Inversion Structure and Its Controls on Oil and Gas in Jurong Basin of Yangtze Area.Geological Review,61(5):1047~1060.
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