塔里木盆地中央隆起带断裂活动及其对海相克拉通解体的作用
摘要
在地震剖面地质构造解释的基础上,深入分析了塔里木盆地断裂系统在中央隆起带的形成演化及塔里木海相克拉通盆地演化过程中的作用.研究表明,塔里木盆地中央隆起带主要发育中加里东I幕(早奥陶世末)、II幕(晚奥陶世末)和喜马拉雅运动中晚期(中新世末以来)共3期大规模断裂系统.这些断裂系统的活动控制了中央隆起带构造演化过程和隆坳格局的变迁,其中巴楚隆起经历了加里东中晚期隆后斜坡和海西-燕山期前隆,至喜马拉雅运动中晚期最终定型为挤压断隆.塔中隆起形成于中加里东I幕构造运动,至中加里东II幕构造运动定型,而塔东隆起则形成于中加里东II幕构造运动并基本定型;将塔里木古生代海相克拉通盆地的演化过程划分为海相克拉通盆地的形成、解体和消亡(即陆内前陆和挤压坳陷形成)3个演化阶段,认为中加里东两期断裂系统的形成是塔里木海相克拉通解体的重要原因.
Based on elaborate geological structural interpretation of seismic profiles,this paper analyzes in details the controlling of fault activity to development of central uplift zone and marine cratonic evolution of Tarim basin.The research indicates that there are mainly three episodes of fault systems:the middle Caledonian orogeny I episode,the middle Caledonian orogeny II episode and the mid-late Himalayan(since Late Miocene).These fault systems controlled the tectonic evolution of central uplift zone and migration of upliftsag,in which Bachu uplift experienced back-bulge ramp in the mid-late of Caledonian period,forebulge in the Hercynian-Yanshanian period and the latest compressional fault uplift in the mid-late of Himalayan period,Tazhong uplift started at the first episode of Caledonian period and formed at the second episode of Caledonian period and Tadong uplift started and formed at the second episode of Caledonian period.The evolution of marine cratonic basin is divided into three periods which are formation,disintegration and extinction. Analysis shows that the fault system of Caledonian I and Caledonian II episodes resulted in breakup of Tarim marine cratonic basin.
Based on elaborate geological structural interpretation of seismic profiles,this paper analyzes in details the controlling of fault activity to development of central uplift zone and marine cratonic evolution of Tarim basin.The research indicates that there are mainly three episodes of fault systems:the middle Caledonian orogeny I episode,the middle Caledonian orogeny II episode and the mid-late Himalayan(since Late Miocene).These fault systems controlled the tectonic evolution of central uplift zone and migration of upliftsag,in which Bachu uplift experienced back-bulge ramp in the mid-late of Caledonian period,forebulge in the Hercynian-Yanshanian period and the latest compressional fault uplift in the mid-late of Himalayan period,Tazhong uplift started at the first episode of Caledonian period and formed at the second episode of Caledonian period and Tadong uplift started and formed at the second episode of Caledonian period.The evolution of marine cratonic basin is divided into three periods which are formation,disintegration and extinction. Analysis shows that the fault system of Caledonian I and Caledonian II episodes resulted in breakup of Tarim marine cratonic basin.
引文
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Buslov,M.M.,Fujiwara,Y.,Iwata,K.,et al.,2004.LatePaleozoic-Early Mesozoic geodynamics of Central Asia.Gondwana Research,7(3):791-808.doi:10.1016/S1342-937X(05)71064-9
Carroll,A.R.,Graham,S.A.,Chang,E.Z.,et al.,2001.Sinian through Permian tectonostratigraphic evolutionof the northwestern Tarim basin,China.Geological So-ciety of America Memoir,194:47-69.doi:10.1130/0-8137-1194-0.47
Carroll,A.R.,Graham,S.A.,Smith,M.E.,2010.Walledsedimentary basins of China.Basin Research,22(1):17-32.doi:10.1111/j.1365-2117.2009.00458.x
Chen,H.L.,Luo,J.C.,Guo,Q.Y.,et al.,2009.Deforma-tion history and tectonic evolution of southeastern Tar-im basin in Mesozoic and Cenozoic.Geotectonica et Met-allogenia,33(1):38-45(in Chinese with English ab-stract).
Ding,W.L.,Lin,C.S.,Qi,L.X.,et al.,2008.Structuralframework and evolution of Bachu uplift in Tarim ba-sin.Earth Science Frontiers,15(2):242-252(in Chi-nese with English abstract).
He,D.F.,Zhou,X.Y.,Zhang,C.J.,et al.,2006.Character-istics of geologic framework of multicycle superimposed basin in Tarim basin.China Petroleum Exploration,11(1):31-41(in Chinese with English abstract).
He,Z.L.,Xu,H.J.,Duan,T.J.,2005.A prelimimary analy-sis on compound structural styles in the Tarim polycy-clic basin.Chinese Journal of Geology,40(2):153-166(in Chinese with English abstract).
Jia,C.Z.,2004a.Tectonic feature and hydrocarbon of TarimMesozoic-Cenozoic basin.Petroleum Industry Press,Beijing(in Chinese).
Jia,C.Z.,2004b.Plate tectonic and continental dynamics ofthe Tarim basin.Petroleum Industry Press,Beijing(inChinese).
Kang,Y.Z.,Wang,Z.X.,2009.Research on oil-controllingof tectonic systems in Tarim basin.China Land Press,Beijing(in Chinese).
Li,B.L.,Guan,S.W.,Li,C.X.,et al.,2009.Paleo-tectonicevolution and deformation features of the lower uplift inthe central Tarim basin.Geological Review,55(4):521-530(in Chinese with English abstract).
Li,Y.J.,Wu,G.Y.,Meng,Q.L.,et al.,2008.Fault sys-tems in central area of the Tarim basin:geometry,kine-matics and dynamic settings.Chinese Journal of Geolo-gy,43(1):82-118(in Chinese with English ab-stract).
Lin,C.S.,Li,S.T.,Liu,J.Y.,et al.,2011.Tectonic frame-work and paleogeographic evolution of the Tarim basinduring the Paleozoic major evolutionary stages.ActaPetrologica Sinica,27(1):210-218(in Chinese withEnglish abstract).
Lin,C.S.,Yang,H.J.,Liu,J.Y.,et al.,2008.Paleohigh ge-omorphology and paleogeographic framework and theircontrols on the formation and distribution of strati-graphic traps in the Tarim basin.Oil &Gas Geology,29(2):189-197(in Chinese with English abstract).
en,J.Y.,Hu,D.S.,Yang,H.Z.,et al.,2011a.Fault sys-tem and its control of carbonate platform in Tazhonguplift area,Tarim basin.Geologyin China,38(4):935-944(in Chinese with English abstract).
Ren,J.Y.,Zhang,J.X.,Yang,H.Z.,et al.,2011b.Analysisof fault systems in the central uplift,Tarim basin.ActaPetrologica Sinica,27(1):219-230(in Chinese withEnglish abstract).
Sun,L.D.,Li,Y.J.,Jiang,T.W.,et al.,2007.The centralTarim lower uplift:a composite hydrocarbon accumula-tion play in the Tarim basin,NW China.Chinese Jour-nal of Geology,42(3):602-620(in Chinese withEnglish abstract).
Tang,L.J.,Jia,C.Z.,Jin,Z.J.,et al.,2003.The main tec-tonic characteristics of superimposed basins,NorthwestChina.Earth Science Frontiers,10(Special):118-124(in Chinese with English abstract).
Windley,B.F.,Alexeiev,D.,Xiao,W.J.,et al.,2007.Tec-tonic models for accretion of the Central Asian orogenicbelt.Journal of Geological Society,164(1):31-47.doi:10.1144/0016-76492006-022
Xiao,A.C.,Yang,S.F.,Li,Y.J.,et al.,2005.Main periodfor creation of fracture system in the Bachu uplift,Tar-im basin.Chinese Journal of Geology,40(2):291-302(in Chinese with English abstract).
Xu,Z.Q.,Li,S.T.,Zhang,J.X.,et al.,2011.Paleo-Asianand Tethyan tectonic systems with docking the Tarimblock.Acta Petrologica Sinica,27(1):1-22(in Chi-nese with English abstract).
Yang,S.F.,Chen,L.F.,Xiao,Z.Y.,et al.,2009.The Ce-nozoic fault systems of southeastern Tarim basin.Geo-tectonica et Metallogenia,33(1):33-37(in Chinesewith English abstract).
陈汉林,罗俊成,郭群英,等,2009.塔里木盆地东南缘中新生代变形史与构造演化.大地构造与成矿学,33(1):38-45.
丁文龙,林畅松,漆立新,等,2008.塔里木盆地巴楚隆起构造格架及形成演化.地学前缘,15(2):242-252.
何登发,周新源,张朝军,等,2006.塔里木多旋回叠合盆地地质结构特征.中国石油勘探,11(1):31-41.
何治亮,徐宏节,段铁军,2005.塔里木多旋回盆地复合构造样式初步分析.地质科学,40(2):153-166.
贾承造,2004a.塔里木盆地中新生代构造特征与油气.北京:石油工业出版社.
贾承造,2004b.塔里木盆地板块构造与大陆动力学.北京:石油工业出版社.
康玉柱,王宗秀,2009.塔里木盆地构造体系控油作用研究.北京:中国大地出版社.
李本亮,管树巍,李传新,等,2009.塔里木盆地塔中低凸起古构造演化与变形特征.地质评论,55(4):521-530.
李曰俊,吴根耀,孟庆龙,等,2008.塔里木盆地中央地区的断裂系统:几何学、运动学和动力学背景.地质科学,43(1):82-118.
林畅松,李思田,刘景彦,等,2011.塔里木盆地古生代重要演化阶段的古构造格局与古地理演化.岩石学报,27(1):210-218.
林畅松,杨海军,刘景彦,等,2008.塔里木早古生代原盆地古隆起地貌和古地理格局与地层圈闭发育分布.石油与天然气地质,29(2):189-197.
任建业,胡德胜,阳怀忠,等,2011a.塔中隆起带断裂系统及其对碳酸盐岩台地的控制.中国地质,38(4):935-944.
任建业,张俊霞,阳怀忠,等,2011b.塔里木盆地中央隆起带断裂系统分析.岩石学报,27(1):219-230.
孙龙德,李曰俊,江同文,等,2007.塔里木盆地塔中低凸起:一个典型的复式油气聚集区.地质科学,42(3):602-620.
汤良杰,贾承造,金之钧,等,2003.中国西北叠合盆地的主要构造特征.地学前缘,10(特刊):118-124.
肖安成,杨树峰,李曰俊,等,2005.塔里木盆地巴楚隆起断裂系统主要形成时代的新认识.地质科学,40(2):291-302.
许志琴,李思田,张建新,等,2011.塔里木地块与古亚洲/特提斯构造体系的对接.岩石学报,27(1):1-22.
杨树峰,陈立峰,肖中尧,等,2009.塔里木盆地东南缘新生代断裂系统.大地构造与成矿学,33(1):33-37.
Buslov,M.M.,Fujiwara,Y.,Iwata,K.,et al.,2004.LatePaleozoic-Early Mesozoic geodynamics of Central Asia.Gondwana Research,7(3):791-808.doi:10.1016/S1342-937X(05)71064-9
Carroll,A.R.,Graham,S.A.,Chang,E.Z.,et al.,2001.Sinian through Permian tectonostratigraphic evolutionof the northwestern Tarim basin,China.Geological So-ciety of America Memoir,194:47-69.doi:10.1130/0-8137-1194-0.47
Carroll,A.R.,Graham,S.A.,Smith,M.E.,2010.Walledsedimentary basins of China.Basin Research,22(1):17-32.doi:10.1111/j.1365-2117.2009.00458.x
Chen,H.L.,Luo,J.C.,Guo,Q.Y.,et al.,2009.Deforma-tion history and tectonic evolution of southeastern Tar-im basin in Mesozoic and Cenozoic.Geotectonica et Met-allogenia,33(1):38-45(in Chinese with English ab-stract).
Ding,W.L.,Lin,C.S.,Qi,L.X.,et al.,2008.Structuralframework and evolution of Bachu uplift in Tarim ba-sin.Earth Science Frontiers,15(2):242-252(in Chi-nese with English abstract).
He,D.F.,Zhou,X.Y.,Zhang,C.J.,et al.,2006.Character-istics of geologic framework of multicycle superimposed basin in Tarim basin.China Petroleum Exploration,11(1):31-41(in Chinese with English abstract).
He,Z.L.,Xu,H.J.,Duan,T.J.,2005.A prelimimary analy-sis on compound structural styles in the Tarim polycy-clic basin.Chinese Journal of Geology,40(2):153-166(in Chinese with English abstract).
Jia,C.Z.,2004a.Tectonic feature and hydrocarbon of TarimMesozoic-Cenozoic basin.Petroleum Industry Press,Beijing(in Chinese).
Jia,C.Z.,2004b.Plate tectonic and continental dynamics ofthe Tarim basin.Petroleum Industry Press,Beijing(inChinese).
Kang,Y.Z.,Wang,Z.X.,2009.Research on oil-controllingof tectonic systems in Tarim basin.China Land Press,Beijing(in Chinese).
Li,B.L.,Guan,S.W.,Li,C.X.,et al.,2009.Paleo-tectonicevolution and deformation features of the lower uplift inthe central Tarim basin.Geological Review,55(4):521-530(in Chinese with English abstract).
Li,Y.J.,Wu,G.Y.,Meng,Q.L.,et al.,2008.Fault sys-tems in central area of the Tarim basin:geometry,kine-matics and dynamic settings.Chinese Journal of Geolo-gy,43(1):82-118(in Chinese with English ab-stract).
Lin,C.S.,Li,S.T.,Liu,J.Y.,et al.,2011.Tectonic frame-work and paleogeographic evolution of the Tarim basinduring the Paleozoic major evolutionary stages.ActaPetrologica Sinica,27(1):210-218(in Chinese withEnglish abstract).
Lin,C.S.,Yang,H.J.,Liu,J.Y.,et al.,2008.Paleohigh ge-omorphology and paleogeographic framework and theircontrols on the formation and distribution of strati-graphic traps in the Tarim basin.Oil &Gas Geology,29(2):189-197(in Chinese with English abstract).
en,J.Y.,Hu,D.S.,Yang,H.Z.,et al.,2011a.Fault sys-tem and its control of carbonate platform in Tazhonguplift area,Tarim basin.Geologyin China,38(4):935-944(in Chinese with English abstract).
Ren,J.Y.,Zhang,J.X.,Yang,H.Z.,et al.,2011b.Analysisof fault systems in the central uplift,Tarim basin.ActaPetrologica Sinica,27(1):219-230(in Chinese withEnglish abstract).
Sun,L.D.,Li,Y.J.,Jiang,T.W.,et al.,2007.The centralTarim lower uplift:a composite hydrocarbon accumula-tion play in the Tarim basin,NW China.Chinese Jour-nal of Geology,42(3):602-620(in Chinese withEnglish abstract).
Tang,L.J.,Jia,C.Z.,Jin,Z.J.,et al.,2003.The main tec-tonic characteristics of superimposed basins,NorthwestChina.Earth Science Frontiers,10(Special):118-124(in Chinese with English abstract).
Windley,B.F.,Alexeiev,D.,Xiao,W.J.,et al.,2007.Tec-tonic models for accretion of the Central Asian orogenicbelt.Journal of Geological Society,164(1):31-47.doi:10.1144/0016-76492006-022
Xiao,A.C.,Yang,S.F.,Li,Y.J.,et al.,2005.Main periodfor creation of fracture system in the Bachu uplift,Tar-im basin.Chinese Journal of Geology,40(2):291-302(in Chinese with English abstract).
Xu,Z.Q.,Li,S.T.,Zhang,J.X.,et al.,2011.Paleo-Asianand Tethyan tectonic systems with docking the Tarimblock.Acta Petrologica Sinica,27(1):1-22(in Chi-nese with English abstract).
Yang,S.F.,Chen,L.F.,Xiao,Z.Y.,et al.,2009.The Ce-nozoic fault systems of southeastern Tarim basin.Geo-tectonica et Metallogenia,33(1):33-37(in Chinesewith English abstract).
陈汉林,罗俊成,郭群英,等,2009.塔里木盆地东南缘中新生代变形史与构造演化.大地构造与成矿学,33(1):38-45.
丁文龙,林畅松,漆立新,等,2008.塔里木盆地巴楚隆起构造格架及形成演化.地学前缘,15(2):242-252.
何登发,周新源,张朝军,等,2006.塔里木多旋回叠合盆地地质结构特征.中国石油勘探,11(1):31-41.
何治亮,徐宏节,段铁军,2005.塔里木多旋回盆地复合构造样式初步分析.地质科学,40(2):153-166.
贾承造,2004a.塔里木盆地中新生代构造特征与油气.北京:石油工业出版社.
贾承造,2004b.塔里木盆地板块构造与大陆动力学.北京:石油工业出版社.
康玉柱,王宗秀,2009.塔里木盆地构造体系控油作用研究.北京:中国大地出版社.
李本亮,管树巍,李传新,等,2009.塔里木盆地塔中低凸起古构造演化与变形特征.地质评论,55(4):521-530.
李曰俊,吴根耀,孟庆龙,等,2008.塔里木盆地中央地区的断裂系统:几何学、运动学和动力学背景.地质科学,43(1):82-118.
林畅松,李思田,刘景彦,等,2011.塔里木盆地古生代重要演化阶段的古构造格局与古地理演化.岩石学报,27(1):210-218.
林畅松,杨海军,刘景彦,等,2008.塔里木早古生代原盆地古隆起地貌和古地理格局与地层圈闭发育分布.石油与天然气地质,29(2):189-197.
任建业,胡德胜,阳怀忠,等,2011a.塔中隆起带断裂系统及其对碳酸盐岩台地的控制.中国地质,38(4):935-944.
任建业,张俊霞,阳怀忠,等,2011b.塔里木盆地中央隆起带断裂系统分析.岩石学报,27(1):219-230.
孙龙德,李曰俊,江同文,等,2007.塔里木盆地塔中低凸起:一个典型的复式油气聚集区.地质科学,42(3):602-620.
汤良杰,贾承造,金之钧,等,2003.中国西北叠合盆地的主要构造特征.地学前缘,10(特刊):118-124.
肖安成,杨树峰,李曰俊,等,2005.塔里木盆地巴楚隆起断裂系统主要形成时代的新认识.地质科学,40(2):291-302.
许志琴,李思田,张建新,等,2011.塔里木地块与古亚洲/特提斯构造体系的对接.岩石学报,27(1):1-22.
杨树峰,陈立峰,肖中尧,等,2009.塔里木盆地东南缘新生代断裂系统.大地构造与成矿学,33(1):33-37.
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