塔里木盆地巴楚隆起断裂差异活动特征及成因演化
详细信息 本馆镜像全文    |  推荐本文 | | 获取馆网全文
摘要
巴楚隆起是塔里木盆地重要的含油气构造单元,因其断裂构造特征与演化异常复杂,严重制约了对该地区构造特征及演化的认识和油气勘探工作。本文通过对地震资料精细构造解释,并结合塔里木盆地构造演化背景及最新的钻井、露头等资料,阐明了巴楚隆起断裂活动具有明显的分期差异性和分区、分带、分段及分层差异性。巴楚隆起断裂构造主要经历了4期差异活动,即加里东早期发育张扭性断裂、海西晚期断裂挤压反转、喜马拉雅山中期断裂强烈压扭逆冲与分区差异变形、喜马拉雅山晚期西南缘断裂带分段分层差异改造与叠加。断裂演化主要受控于加里东早期、海西晚期和喜马拉雅山中-晚期构造运动及对应时期塔里木古陆周缘洋盆开合与造山作用,喜马拉雅山中期是巴楚隆起断裂活动关键期,因受西昆仑和西南天山强烈挤压,隆起西段发生"屈服型"冲断隆升与走滑旋转,东段相应发生"受限型"弧形逆冲与向南掀斜;喜马拉雅山晚期断裂主要活动表现在隆起西北缘和西南缘,特别在西南缘断裂带发生了强烈的分段、分层差异叠加改造,其成因与西昆仑强烈隆升和向北挤压密切相关。
The Bachu Uplift is one of the most important oil and gas exploration area in the Tarim Basin,but the realization of its structure characteristics and evolution as well as the oil and gas exploration are serious constrained by its exceptionally complex faults structure and evolution.Based on the fine structural interpretation of seismic data,the tectonic setting of Traim Basin's evolution,the new wells data and outcrops,the paper reveals that the activity characteristics of the faults in Bachu Uplift has great difference in different period,different area,and different fault belt,different parts of the same fault,different stratigraphic.There are mainly four periods of the faults' differential activities:Transtensional faults activities in Early Caledonian,positive inversion of early transtensional faults in Late Hercynian,strong strike-slip and thrust and different deform in Middle Himalayan,different transformation and superposition in different parts and stratigraphic in the southwest faults belt in Late Himalayan.Fault evolution is mainly controlled by the tectonic movements of the Early Caledonian,the Late Hercynian and the Middle-Late Himalayan,as well as the opening and closing of oceans surrounding the Tarim paleo-continent and the orogenic movements in the corresponding period.The Middle Himalayan is the critical period for faults activities in the Bachu Uplift,because of the strong compressive stress come from the West Kunlun Mountains and the Southwest Tianshan Mountains,faults in the western part thrust uplift and strike-slip rotation,faults in the eastern part thrust like an arc and tilting to the southward.The Late Himalayan is the deformation period of the faults and it mainly occurs in the northwest edge and the southwest edge of Bachu Uplift,especially in the southwest edge,because of the strong compressive stress comes from the West Kunlun Mountains,strong different deformation and superposition occur in different parts of the southwest faults belt.
引文
曹自成,杜永明,岳勇.2009.巴楚隆起色力布亚断裂活动及其控油作用.断块油气田,16(3):5—7.Cao Zicheng,Du Yongming and Yue Yong.2009.Selibuya fault activity and its control on oil and gas in Bachu Uplift.Faultblock Oil&Gas Field,16(3),5—7.
    陈汉林,杨树锋,董传万等.1997.塔里木盆地地质热事件研究.科学通报,42(10):1096—1098.Chen Hanlin,Yang Shufeng.Dong Chuanwan et al.1997.Geological thermal events in Tarim Basin.Chinese Science Bulletin,42(7):580—584.
    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.Ding Wenlong,Lin Changsong,Qi Lixin et al.2008.Structural framework and evolution of Bachu Uplift in Tarim Basin.Earth Science Frontiers,15(2):242—252.
    付建奎,张光亚,马郡等.1999.塔里木盆地巴楚地区构造样式与演化.石油勘探与开发,26(5):10—11.Fu Jiankui,Zhang Guangya,Ma Jun et al.1999.The structural styles and their evolution in Bachu area of Tarim Basin.Petroleum Exploration and Development,26(5):10—11.
    郭彦如,陈文,穆剑等.2002.阿尔金断裂系及其邻区中—新生代构造演化.地质论评,48(增刊):176—182.Guo Yanru.Chen Wen,Mu Jian et al.2011.Tectonic evolution of the Altun fault system and its adjacent areas in the MesoCenozoic.Geological Review,48(suppl.):176—182.
    何登发,贾承造,李德生等.2005.塔里木盆地多旋回叠合盆地的形成与演化.石油与天然气地质,26(1):64—77.He Dengfa,Jia Chengzao,Li Desheng et al.2005.Formation and evolution of polycyclic superimposed Tarim Basin.OU&Gas Geology,26(1):64—77.
    何碧竹,焦存礼,许志琴等.2011.阿尔金—西昆仑加里东中晚期构造作用在塔里木盆地塘古兹巴斯凹陷中的响应.岩石学报,27(11):3435—3448.He Bizhu,Jiao Cunli,Xu Zhiqin et al.2011.Manifestation of the Middle-Late Caledonian tectonic movement along the AltunWest Kunlun orogenic belt in the Tangguzibas depression,Tarim Basin.Acta Petrologica Sinica,27(11):3435—3448.
    何文渊,李江海,钱祥麟等.2000.塔里木盆地巴楚断隆中新生代的构造演化.北京大学学报(自然科学版),36(4):539—546.Hw Wenyuan.Li Jianghai,Qian Xianglin et al.2000.The Meso-Cenozoic evolution of Bachu fault-uplift in Tarim Basin.Acta Scientiarum Naturalium Vniversitatis Pekinensis,36(4):539—546.
    贾承造,何登发,陆洁民.2004.中国喜马拉雅运动的期次及其动力学背景.石油与天然气地质,25(2):121—125.Jia Chengzao,He Dengfa and Lu Jiemin.2004.Episodes and geodynamic setting of Himalayan movement in China.OU&Gas Geology,25(2):11—125.
    吕海涛,张仲培,邵志兵等.2010.塔里木盆地巴楚—麦盖提地区早古生代古隆起的演化及其勘探意义.石油与天然气地质,31(1):76—90.Lu Haitao,Zhang Zhongpei,Shao Zhibing et al.2010.Structural evolution and exploration significance of the Early Paleozoic palaeouplifts in Bachu-Maigaiti area,the Tarim Basin.Oil&Gas Geology,31(1):76—90.
    刘高波,施泽进,余晓宇.2004.巴楚—麦盏提的区域构造演化与油气分布规律.成都理工大学学报(自然科学版),31(2):157—161.Liu Gaobo,Shi Zejin and She Xiaoyu.2004.Regional tectonic evolution and distribution of Bachu-Markit.Journal of Chengdu University of Technology(Science&Technology Edition),31(2):157—161.
    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.Li Yuejun,Wu Genyao,Meng Qinglong et al.2008.Fault systems in central area of the Tarim Basin:Geometry,kinematics and dynamic settings.Chinese Journal of Geology,43(1):82—118.
    罗廷辉,赵锡奎,李坤等.2010.巴楚隆起色力布亚断裂演化及其油气意义.重庆科技学院学报(自然科学版),12(6):5—8.Luo Tinghui.Zhao Xikui.Li Kun et al.2005.Evolution and its oil-gas sense of Serikbuya fault in Bachu Uplift.Journal of Chongqing University of Science and Technology(Natural Sciences Edition),12(2):291—302.
    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.Lin Changsong.Li Sitian.Liu Jingyan et al.2011.Tectonic framework and paleogeographic evolution of the Tarim Basin during the Paleozoic major evolutionary stages.Acta Petrologica Sinica,27(1):210—218.
    宁飞,汤良杰,朱传玲等.2009.挤压区局部构造转换带类型及石油地质意义.现代地质,23(3):394—400.Ning Fei,Tang Liangjie,Zhu Chuanling et al.2009.Types of structural transfer zone in compressional area and its significance of petroleum geology.Geoscience,23(3):394—400.
    刘志宏,王文革,林东成等.2003.塔里木盆地吐木休克断裂带断层封闭性研究.吉林大学学报(地球科学版),33(1):19—25.Liu Zhihong,Wang Wenge,Lin Dongcheng et al.2003.Study on the faults sealing properties of Tumuxiuke fault belt in Tarim Basin.Journal of Jilin University(Earth Science Edition),33(1):19—25.
    孟庆龙,李曰俊,师骏等.2008a.塔里木盆地西部色力布亚断裂和康西断裂的主要特征及活动时代.地质科学,43(2):282—293.Meng Qinglong,Li Yuejun,Shi Jun et al.2008a.Main characters and active ages of the Serikbuya and Kangxi faults in the western Tarim Basin.Chinese Journal of Geology,43(2):282—293.
    孟庆龙,李曰俊,敬兵等.2008b.塔里木盆地西部巴什托普断裂的主要特征及其油气勘探意义.地质科学,43(3):569—575.Meng Qinglong.Li Yuejun,Jing Bing et al.2008b.Main characteristics of the Bashituopu fault and its petroleum potential in the western Tarim Basin.Chinese Journal of Geology,43(3):569—575.
    曲国胜,李亦纲,陈杰等.2003.柯坪塔格推覆构造几何学、运动学及其构造演化.地学前缘,10(增刊):142—152.Qu Guosheng,Li Yigang,Chen Jie et al.2003.Geometry,kinematics and tectonic evolution of Kepingtage thrust system.Earth Science Frontiers,10(suppl.):142—152.
    任建业,张俊霞,阳怀忠等.2011.塔里木盆地中央隆起带断裂系统分析.岩石学报,27(1):219—230.Ren Jianye,Zhang Junxia,Yang Huaizhong et al.2011.Analysis of fault systems in the central uplift,Tarim Basin.Acta Petrologica Sinica,21(1):219—230.
    汤良杰.1994.塔里术盆地构造演化与构造样式.地球科学,19(6):742—754.Tang Liangjie.1994.Evolution and tectonic patterns of Tarim Basin.Earth.Science,19(6):742—754.
    王清华.1999.塔里木盆地巴楚凸起构造特征及其对油气藏分布的控制.新疆石油地质.20(3):208—209.Wang Qinghua.1999.Structural characteristics and its control on reservoir distribution in Bachu Arch,Tarim Basin.Xinjiang Petroleum Geology,20(3):208—209.
    王宏语,樊太亮,魏福军等.2004.塔里木盆地巴楚中部地区寒武系盐下构造发育特征.石油与天然气地质,25(5):554—558.Wang Hongyu.Fan Tailiang.Wei Fujun et al.2004.Developmental characteristics of Cambrian subsalt structures in Central Bachu area,Tarim Basin.Oil&Gas Geology,25(5):554—558.
    肖安成,李景义,张春生.1998.塔里木盆地色力布亚断裂系的走滑双重构造特征.江汉石油学院学报,20(2):9—15.Xiao Ancheng,Li Jingyi and Zhang Chunsheng.1998.Structure and kinematic genes of the Selibuya strike-slip duplex in the Tarim Basin.Journal of Jianghan Petroleum Institute,20(2):9—15.
    肖安成,杨树锋,李曰俊等.2005a.塔里木盆地巴楚—柯坪地区新生代断裂系统.石油与天然气地质,26(1):78—85.Xiao Ancheng.Yang Shufeng.Li Yuejun et al.2005a.A studying of Cenozoic fracture systems in Bachu-Kalpin area,Tarim Basin.Oil&Gas Geology,26(1):78—85.
    肖安成,杨树锋,李曰俊等.2005b.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,Xiao Ancheng,Yang Shufen.Li Yuejun et al.2005b.Main period for creation of fracture system in the Bachu Uplift,Tarim Basin.Chinese Journal of Geology,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.Xu Zhiqin,Li Sitian,Zhang Jianxin et al.2011.Paleo-Asian and Tethyan tectonic systems with docking the Tarim Block.Acta Petrologica Sinica,27(1):1—22.
    杨庚,石昕,贾承造等.2008.塔里木盆地西北缘柯坪—巴楚地区皮羌断裂与色力布亚断裂空间关系.铀矿地质,24(4):201—207.Yang Geng,Shi Xin.Jia Chengzao et al.2008.Spatial relationship between Piqiang fault and Selibuya fault in Keping-Bachu district,Northwest Tarim Basin.Uranium Geology,24(4):201—207.
    杨明慧,金之钧,吕修祥等.2007.塔里木盆地基底卷入扭压构造与巴楚隆起的形成.地质学报,81(2):158—165.Yang Minghui,Jin Zhijun.L(u|¨)Xiuxiang et al.2007.Basement-involved transpressional structure and the formation of the Bachu Uplift,Tarim Basin,northwestern China.Acta Geologica Sinica,81(2);158—165.
    杨海军,李曰俊,冯晓军等.2007.塔里木盆地玛扎塔格构造带断裂构造分析.地质科学,42(3):506—517.Yang Haijun,Li Yuejun,Feng Xiaojun et al.2007.Analysis on thru stings of the Mazhatage structural belt in the Tarim Basin.Chinese Journal of Geology,42(3):506—517.
    张恺.1990.论塔里木盆地类型、演化特征及含油气远景评价.石油与天然气地质,11(1):1—15.Zhang Kai.1990.On the basin type,evolution feature and petroleum potential of Tarim Basin.Oil&Gas Geology,11(1):1—15.
    朱德丰,刘和甫,吴根耀.2008.塔里术盆地西部吐木休克断裂带的主要特征和构造演化.地质科学,43(2):209—227.Zhu Defeng,Liu Hefu and Wu Genyao.2008.Main characteristics and structural evolution of the Tumxuk fault zone in the western Tarim Basin.Chinese Journal of Geology,43(2):209—227.
    赵明,孙兆玉,岳勇等.2008.巴楚隆起西段色力布亚断裂演化及其封闭性研究.石油天然气学报,30(4):28—32.Zhao Ming,Sun Zhaoyu,Yue Yong et al.2008.Evolution and sealing research of Selibuya fault in the west of Bachu Uplift.Journal of Oil and Gas Technology,30(4):28—32.
    张洪安,吴根耀,李曰俊等.2011.塔里木盆地西部巴楚断隆南界断裂带的主要特征和构造演化.地质通报,30(10):1547—1556.Zhang Hongan,Wu Genyao,Li Yuejun et al.2011.Main features and structural evolution of southern boundary fractural zone of the Bachu fault-rise in western Tarim Basin.Geological Bulletin of China,30(10):1547—1556.
    张一伟,金之钧,刘国臣等.2000.塔里木盆地环满加尔地区主要不整合形成过程及剥蚀量研究.地学前缘,7(4):449—457.Zhang Yiwei,Jin Zhijun,Liu Guochen et al.2000.Study on the formation of unconformaties and the amount of eroded sedimentation in Tarim Basin.Earth Science Frontiers,7(4):449—457.
    Allen M B and Vincent S J.1999.Late Cenozoic tectonics of the Kepingtage thrust zone:Interactions of the Tien Shan and Tarim Basin,Northwest China.Tectonics,18(4):639—654.
    Burtman V S.2000.Cenozoic crustal shortening between the Pamir and Tien Shan and a reconstruction of the Pamir-Tien Shan transition zone for the Cretaceous and Palaeogene.Tectonophysics,319(2):69—92.
    Gao Z Q and Fan T L.2012.Extensional tectonics and sedimentary response of the Early-Middle Cambrian passive continental margin,Tarim Basin,Northwest China.Geoscience Frontiers,3(5):661—668.

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