塔里木盆地巴楚隆起构造格架及形成演化
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摘要
巴楚隆起是塔里木盆地重要的油气勘探地区之一。文中基于新的地震、航磁、重力等资料解释结果和区域构造演化剖面,重新分析了巴楚隆起的构造格架及形成演化。研究认为:巴楚隆起在剖面上为压扭性断裂控制的"两断夹一隆"构造样式,在平面上具有"东西分区、南北分带"的构造格局。此与塔里木盆地断裂构造体系的展布、基底结构与构造、地壳深部地质背景及古构造应力场演变等关系密切。该隆起是一个从震旦纪开始发育演化的继承性活动型古隆起,其形成演化经历了加里东构造旋回阶段(Z—D2)、海西构造旋回阶段(D3—P)、印支—燕山构造旋回阶段(T—K)和喜马拉雅构造旋回阶段(E—Q)。这一新认识对巴楚地区的油气勘探部署和潜力评价均具有重要指导作用。
The Bachu uplift is one of the most important oil and gas exploration area in the Tarim basin.Based on the new results of seismic,aeromagnetic and gravity data interpretation,and on regional tectonic evolution of the profiles,we re-analyze the tectonic framework of the Bachu uplift and the evolution of its formation.The study reveals that the Bachu uplift shows a structural style of "one uplift between two faults" in the profile,which is controlled by the compresso-shear faults,and that it shows a structural pattern of "zoned from east to west,divided into bands from north to south" in the plane,which is closely related to the distribution of fault structure system in the Tarim basin,the basal structures and tectonics,the geological background of deep crust and the evolution of the palaotectonic stress field.The uplift is an inherited mobile paleouplift that began its development and evolution in the Sinian.Its formation and evolution experienced the stage of Caledonian tectonic cycle(Z-D2),the stage of Hercynian tectonic cycle(D3-P),the stage of Indo-Yanshan tectonic cycle(T-K) and the stage of Himalayan tectonic cycle(E-Q).This new understanding is of great guiding significance in the deployment of oil and gas exploration and the evaluation of potentiality.
The Bachu uplift is one of the most important oil and gas exploration area in the Tarim basin.Based on the new results of seismic,aeromagnetic and gravity data interpretation,and on regional tectonic evolution of the profiles,we re-analyze the tectonic framework of the Bachu uplift and the evolution of its formation.The study reveals that the Bachu uplift shows a structural style of "one uplift between two faults" in the profile,which is controlled by the compresso-shear faults,and that it shows a structural pattern of "zoned from east to west,divided into bands from north to south" in the plane,which is closely related to the distribution of fault structure system in the Tarim basin,the basal structures and tectonics,the geological background of deep crust and the evolution of the palaotectonic stress field.The uplift is an inherited mobile paleouplift that began its development and evolution in the Sinian.Its formation and evolution experienced the stage of Caledonian tectonic cycle(Z-D2),the stage of Hercynian tectonic cycle(D3-P),the stage of Indo-Yanshan tectonic cycle(T-K) and the stage of Himalayan tectonic cycle(E-Q).This new understanding is of great guiding significance in the deployment of oil and gas exploration and the evaluation of potentiality.
引文
[1]林畅松,丁文龙,刘景彦.塔里木盆地形成演化和构造作用.中国地质大学(北京),2007.
[2]何毅,冀连胜.塔里木盆地重磁电资料综合解释成果.石油物探局五处,2000.
[3]王宜昌,程正发,刘玮.塔西南—巴楚地区综合物化探研究及勘探方向预测.北京地大惠信科技发展有限公司,2004.
[1]Jia C Z.Structural characteristics and oil and gas in Tari m basin of China[M].Beijing:PetroleumIndustry Press,1997(in Chinese).
[2]Li D C,Ji L S.Comprehensive study of non-seismic data in Tari mbasin and the piedmont with peripheral[M].Beijing:PetroleumIndustry Press,2003(in Chinese).
[3]Zuo L P,Li T,Cao Y.Structural characteristics of Bachu arch andits petroliferous prospects in Tari m basin[J].Xin-jiang Petroleum Geology,2001,22(5):411-413(in Chinese).
[4]Jia C Z,Yao HJ,Wei G Q,et al.Plate tectonic evolution and tectonic features of major tectonic units in Tari m basin[C]∥Tong X G,Liang D G.Collection of oil and gas explo-ration in Tari m basin.rmqi:Xinjiang Technology and Health,1992(in Chinese).
[5]Wang Q H.Structural characteristics and its control on res-ervoir distribution in Bachu arch,Tari m basin[J].Xinjiang Petroleum Geology,1999,20(3):208-209(in Chinese).
[6]Li H H,Zhang G Y,Liu J X,et al.Hydrocarbon prospec-ting model in Bachu faulted uplift,Tari m basin[J].Petrole-um Exploration and Development,1998,25(5):11-13(in Chi-nese).
[7]Jia C Z,Wei G Q,Yao HJ,et al.Basin tectonic evolution and regional tectonic geology[M]∥Tong X G,Liang D G.Series of oil and gas exploration in Tari m basin.Beijing:Pe-troleumIndustry Press,1995(in Chinese).
[8]Kang Y Z,Kang Z H.Tectonic evolution and oil and gas of Tarin basin[J].Bulletin of the Chinese Academy of Geolog-ical Sciences,1994,3(4):180-191(in Chinese).
[9]He D F,Li D S.Tari m basin tectonic evolution and hydro-carbon accumulation[M].Beijing:Geological Publishing House,1996(in Chinese).
[10]He D F,Jia C Z,Li D S,et al.Formation and evolution of polycyclic superi mposed Tari mbasin[J].Oil&Gas Geology,2005,26(1):64-77(in Chinese).
[11]Fu J K,Zhang G Y,Ma J,et al.The structural styles and their evolution in Bachu area of Tari m basin[J].Petroleum Exploration and Development,1999,26(5):10-11(in Chi-nese).
[12]Liu G B,Shi Z J,She X Y.Regional tectonic evolution and distribution of Bachu-Markit[J].Journal of Chengdu Univer-sity of Technology:Science and Technology Edition,2004,36(2):157-161(in Chinese).
[13]He W Y,Li J H,Qian X L,et al.The Meso-Cenozoic evolu-tion of Bachu fault-uplift in Tari m basin[J].Acta Scicentia-rum Naturalum Universitis Pekinesis,2000,36(4):539-545(in Chinese).
[14]Yang KS.Tectonic evolution of Tari mbasin[J].Marine Ge-ology Letters,2005,21(2):25-29(in Chinese).
[15]Zhang G Y.Formation and evolution of Paleozoic craton ba-sin and oil and gas in Tari m basin[M].Beijing:Geological Publishing House,2000(in Chinese).
[16]Tang LJ.Evolution andtectonic patterns of Tari mbasin[J].Earth Science—Journal of China University of Geosciences,1994,19(6):742-754(in Chinese).
[17]Tang L J.An approach to major tectogenesis of Tari m basin[J].Petroleum Geology&Experi ment,1997,19(2):108-114(in Chinese).
[18]Liu X,GrahamS,Chang E,et al.Tectonic evolution of Tar-i m plate and its surrounding area since Late Paleozoic[J].Earth Science—Journal of China University of Geosciences,1994,19(6):715-725(in Chinese).
[19]Zhang Z M,Jia C Z.Palaeohighs in craton basin of Tari m and the exploration objectives[J].Journal of Xi an Shiyou U-niversity,1997,12(3):8-13(in Chinese).
[20]Xu X H.Formation of paleo-uplift and petroleumoccurrence in Tari mbasin[J].Journal of Tongji University:Natural Sci-ence Edition,2004,32(4):461-465(in Chinese).
[21]Li YJ,Mai G R,Luo J C,et al.Palaeozoic tectonic setting and provenance nature discri mination of Bachu fault-uplift,Tari m,Northwest China[J].Journal of Palaeogeography,1999,1(4):45-52(in Chinese).
[22]Xie X A,Wu Q Z,Lu H F.Tectonic framework and sedi-mentary feature of the Tari mbasinin Paleozoic[J].Sedmien-tologica Transaction,1997,15(1):152-155(in Chinese).
[23]Xie X A,Hu S Y,Lu H F.Positive inversion structure in the Bachu fault-uplift in the Tari m basin[J].Geological Re-view,1998,44(1):1-5(in Chinese).
[1]贾承造.中国塔里木盆地构造特征与油气[M].北京:石油工业出版社,1997.
[2]李德春,冀连胜.塔里木盆地及周缘山前带非地震资料综合研究[M].北京:石油工业出版社,2003.
[3]左龙凭,李铁,曹杨.塔里木盆地巴楚凸起构造特征及含油气远景[J].新疆石油地质,2001,22(5):411-413.
[4]贾承造,姚慧君,魏国齐,等.塔里木盆地板块构造演化和主要构造单元地质构造特征[C]∥童晓光,梁狄刚.塔里木盆地油气勘探论文集.乌鲁木齐:新疆科技卫生出版社,1992.
[5]王清华.塔里木盆地巴楚凸起构造特征及其对油气藏分布的控制[J].新疆石油地质,1999,20(3):208-209.
[6]李洪辉,张光亚,刘建新,等.塔里木盆地巴楚断隆油气勘探模式[J].石油勘探与开发,1998,25(5):11-13.
[7]贾承造,魏国齐,姚慧君,等.盆地构造演化与区域构造地质[M]∥童晓光,梁狄刚.塔里木盆地油气勘探丛书.北京:石油工业出版社,1995.
[8]康玉柱,康志宏.塔里木盆地构造演化与油气[J].地球学报,1994,3(4):180-191.
[9]何登发,李德生.塔里木盆地构造演化与油气聚集[M].北京:地质出版社,1996.
[10]何登发,贾承造,李德生,等.塔里木盆地多旋回叠合盆地的形成与演化[J].石油与天然气地质,2005,26(1):64-77.
[11]付建奎,张光亚,马郡,等.塔里木盆地巴楚地区构造样式与演化[J].石油勘探与开发,1999,26(5):10-11.
[12]刘高波,施泽进,佘晓宇.巴楚—麦盖提的区域构造演化与油气分布规律[J].成都理工大学学报:自然科学版,2004,31(2):157-161.
[13]何文渊,李江海,钱祥麟,等.塔里木盆地巴楚断隆中新生代的构造演化[J].北京大学学报:自然科学版,2000,36(4):539-545.
[14]杨克绳.塔里木盆地的构造演化[J].海洋地质动态,2005,21(2):25-29.
[15]张光亚.塔里木盆地古生代克拉通盆地形成演化与油气[M].北京:地质出版社,2000.
[16]汤良杰.塔里木盆地演化和构造样式[J].地球科学——中国地质大学学报,1994,19(6):742-754.
[17]汤良杰.略论塔里木盆地主要构造运动[J].石油实验地质,1997,19(2):108-114.
[18]刘训,GrahamS,Chang E,等.塔里木板块周缘晚古生代以来的构造演化[J].地球科学——中国地质大学学报,1994,19(6):715-725.
[19]张宗命,贾承造.塔里木克拉通盆地内古隆起及其找油方向[J].西安石油学院学报,1997,12(3):8-13.
[20]徐旭辉.塔里木盆地古隆起形成和油气控制[J].同济大学学报:自然科学版,2004,32(4):461-465.
[21]李曰俊,买光荣,罗俊成,等.塔里木盆地巴楚断隆古生代沉积构造背景和物源区性质的探讨[J].古地理学报,1999,1(4):45-52.
[22]谢晓安,吴奇之,卢华复.塔里木盆地古生代构造格架与沉积特征[J].沉积学报,1997,15(1):152-155.
[23]谢晓安,胡素云,卢华复.探讨塔里木盆地巴楚断隆的正反转构造[J].地质论评,1998,44(1):1-5.
[2]何毅,冀连胜.塔里木盆地重磁电资料综合解释成果.石油物探局五处,2000.
[3]王宜昌,程正发,刘玮.塔西南—巴楚地区综合物化探研究及勘探方向预测.北京地大惠信科技发展有限公司,2004.
[1]Jia C Z.Structural characteristics and oil and gas in Tari m basin of China[M].Beijing:PetroleumIndustry Press,1997(in Chinese).
[2]Li D C,Ji L S.Comprehensive study of non-seismic data in Tari mbasin and the piedmont with peripheral[M].Beijing:PetroleumIndustry Press,2003(in Chinese).
[3]Zuo L P,Li T,Cao Y.Structural characteristics of Bachu arch andits petroliferous prospects in Tari m basin[J].Xin-jiang Petroleum Geology,2001,22(5):411-413(in Chinese).
[4]Jia C Z,Yao HJ,Wei G Q,et al.Plate tectonic evolution and tectonic features of major tectonic units in Tari m basin[C]∥Tong X G,Liang D G.Collection of oil and gas explo-ration in Tari m basin.rmqi:Xinjiang Technology and Health,1992(in Chinese).
[5]Wang Q H.Structural characteristics and its control on res-ervoir distribution in Bachu arch,Tari m basin[J].Xinjiang Petroleum Geology,1999,20(3):208-209(in Chinese).
[6]Li H H,Zhang G Y,Liu J X,et al.Hydrocarbon prospec-ting model in Bachu faulted uplift,Tari m basin[J].Petrole-um Exploration and Development,1998,25(5):11-13(in Chi-nese).
[7]Jia C Z,Wei G Q,Yao HJ,et al.Basin tectonic evolution and regional tectonic geology[M]∥Tong X G,Liang D G.Series of oil and gas exploration in Tari m basin.Beijing:Pe-troleumIndustry Press,1995(in Chinese).
[8]Kang Y Z,Kang Z H.Tectonic evolution and oil and gas of Tarin basin[J].Bulletin of the Chinese Academy of Geolog-ical Sciences,1994,3(4):180-191(in Chinese).
[9]He D F,Li D S.Tari m basin tectonic evolution and hydro-carbon accumulation[M].Beijing:Geological Publishing House,1996(in Chinese).
[10]He D F,Jia C Z,Li D S,et al.Formation and evolution of polycyclic superi mposed Tari mbasin[J].Oil&Gas Geology,2005,26(1):64-77(in Chinese).
[11]Fu J K,Zhang G Y,Ma J,et al.The structural styles and their evolution in Bachu area of Tari m basin[J].Petroleum Exploration and Development,1999,26(5):10-11(in Chi-nese).
[12]Liu G B,Shi Z J,She X Y.Regional tectonic evolution and distribution of Bachu-Markit[J].Journal of Chengdu Univer-sity of Technology:Science and Technology Edition,2004,36(2):157-161(in Chinese).
[13]He W Y,Li J H,Qian X L,et al.The Meso-Cenozoic evolu-tion of Bachu fault-uplift in Tari m basin[J].Acta Scicentia-rum Naturalum Universitis Pekinesis,2000,36(4):539-545(in Chinese).
[14]Yang KS.Tectonic evolution of Tari mbasin[J].Marine Ge-ology Letters,2005,21(2):25-29(in Chinese).
[15]Zhang G Y.Formation and evolution of Paleozoic craton ba-sin and oil and gas in Tari m basin[M].Beijing:Geological Publishing House,2000(in Chinese).
[16]Tang LJ.Evolution andtectonic patterns of Tari mbasin[J].Earth Science—Journal of China University of Geosciences,1994,19(6):742-754(in Chinese).
[17]Tang L J.An approach to major tectogenesis of Tari m basin[J].Petroleum Geology&Experi ment,1997,19(2):108-114(in Chinese).
[18]Liu X,GrahamS,Chang E,et al.Tectonic evolution of Tar-i m plate and its surrounding area since Late Paleozoic[J].Earth Science—Journal of China University of Geosciences,1994,19(6):715-725(in Chinese).
[19]Zhang Z M,Jia C Z.Palaeohighs in craton basin of Tari m and the exploration objectives[J].Journal of Xi an Shiyou U-niversity,1997,12(3):8-13(in Chinese).
[20]Xu X H.Formation of paleo-uplift and petroleumoccurrence in Tari mbasin[J].Journal of Tongji University:Natural Sci-ence Edition,2004,32(4):461-465(in Chinese).
[21]Li YJ,Mai G R,Luo J C,et al.Palaeozoic tectonic setting and provenance nature discri mination of Bachu fault-uplift,Tari m,Northwest China[J].Journal of Palaeogeography,1999,1(4):45-52(in Chinese).
[22]Xie X A,Wu Q Z,Lu H F.Tectonic framework and sedi-mentary feature of the Tari mbasinin Paleozoic[J].Sedmien-tologica Transaction,1997,15(1):152-155(in Chinese).
[23]Xie X A,Hu S Y,Lu H F.Positive inversion structure in the Bachu fault-uplift in the Tari m basin[J].Geological Re-view,1998,44(1):1-5(in Chinese).
[1]贾承造.中国塔里木盆地构造特征与油气[M].北京:石油工业出版社,1997.
[2]李德春,冀连胜.塔里木盆地及周缘山前带非地震资料综合研究[M].北京:石油工业出版社,2003.
[3]左龙凭,李铁,曹杨.塔里木盆地巴楚凸起构造特征及含油气远景[J].新疆石油地质,2001,22(5):411-413.
[4]贾承造,姚慧君,魏国齐,等.塔里木盆地板块构造演化和主要构造单元地质构造特征[C]∥童晓光,梁狄刚.塔里木盆地油气勘探论文集.乌鲁木齐:新疆科技卫生出版社,1992.
[5]王清华.塔里木盆地巴楚凸起构造特征及其对油气藏分布的控制[J].新疆石油地质,1999,20(3):208-209.
[6]李洪辉,张光亚,刘建新,等.塔里木盆地巴楚断隆油气勘探模式[J].石油勘探与开发,1998,25(5):11-13.
[7]贾承造,魏国齐,姚慧君,等.盆地构造演化与区域构造地质[M]∥童晓光,梁狄刚.塔里木盆地油气勘探丛书.北京:石油工业出版社,1995.
[8]康玉柱,康志宏.塔里木盆地构造演化与油气[J].地球学报,1994,3(4):180-191.
[9]何登发,李德生.塔里木盆地构造演化与油气聚集[M].北京:地质出版社,1996.
[10]何登发,贾承造,李德生,等.塔里木盆地多旋回叠合盆地的形成与演化[J].石油与天然气地质,2005,26(1):64-77.
[11]付建奎,张光亚,马郡,等.塔里木盆地巴楚地区构造样式与演化[J].石油勘探与开发,1999,26(5):10-11.
[12]刘高波,施泽进,佘晓宇.巴楚—麦盖提的区域构造演化与油气分布规律[J].成都理工大学学报:自然科学版,2004,31(2):157-161.
[13]何文渊,李江海,钱祥麟,等.塔里木盆地巴楚断隆中新生代的构造演化[J].北京大学学报:自然科学版,2000,36(4):539-545.
[14]杨克绳.塔里木盆地的构造演化[J].海洋地质动态,2005,21(2):25-29.
[15]张光亚.塔里木盆地古生代克拉通盆地形成演化与油气[M].北京:地质出版社,2000.
[16]汤良杰.塔里木盆地演化和构造样式[J].地球科学——中国地质大学学报,1994,19(6):742-754.
[17]汤良杰.略论塔里木盆地主要构造运动[J].石油实验地质,1997,19(2):108-114.
[18]刘训,GrahamS,Chang E,等.塔里木板块周缘晚古生代以来的构造演化[J].地球科学——中国地质大学学报,1994,19(6):715-725.
[19]张宗命,贾承造.塔里木克拉通盆地内古隆起及其找油方向[J].西安石油学院学报,1997,12(3):8-13.
[20]徐旭辉.塔里木盆地古隆起形成和油气控制[J].同济大学学报:自然科学版,2004,32(4):461-465.
[21]李曰俊,买光荣,罗俊成,等.塔里木盆地巴楚断隆古生代沉积构造背景和物源区性质的探讨[J].古地理学报,1999,1(4):45-52.
[22]谢晓安,吴奇之,卢华复.塔里木盆地古生代构造格架与沉积特征[J].沉积学报,1997,15(1):152-155.
[23]谢晓安,胡素云,卢华复.探讨塔里木盆地巴楚断隆的正反转构造[J].地质论评,1998,44(1):1-5.
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