塔里木盆地塔中Ⅲ区奥陶系碳酸盐岩油气成藏主控因素及有利区带
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摘要
碳酸盐岩是塔里木盆地塔中地区古生界油气勘探的主要目的层,探讨其成藏主控因素对碳酸盐岩勘探具有重要的意义。针对塔中Ⅲ区油气成藏规律复杂、难以有效拓展的难题,从构造断裂发育演化对碳酸盐岩储层沉积、储层后期改造以及油气运移和聚集的影响入手,明确了受断裂挤压抬升控制的高能相带是岩溶储层发育的物质基础,塔中Ⅲ区广泛发育台内高能滩和台内缓滩;北东向走滑断裂体系羽状破碎带和斜列叠置破碎带是储层最为发育的区域;关键成藏期古构造控制了塔中Ⅲ区古生界油气由北向南的运移路径,鼻状构造区油气运聚有利。在此基础上,结合区域盖层展布特征、储层分类预测结果和实钻油藏特征进行了成藏有利区综合评价,指明了塔中Ⅲ区下步勘探有利方向。
Carbonate rock is the major target horizon for Paleogene oil/gas exploration in the Tazhong area of the Tarim Basin. Study of the major factors controlling reservoir formation plays an important role in carbonate exploration. The complexity of reservoir forming in Tazhong block Ⅲ has restricted exploration,so analysis of carbonate reservoir deposition and later re-formation was carried out in terms of tectonic evolution to confirm that the high-energy facies controlled by faulted uplifting was the material basis for karstification. High-energy shoals and inner platform gentle shoals are widely developed in Tazhong block Ⅲ. The feather-shaped fractured zone and echelon faults in the NE strike-slip fault system are favorable areas for reservoir development. The paleostructures in the crucial period of hydrocarbon accumulation controlled the migration pathway for Paleogene oil/gas migration from north to south in Tazhong block Ⅲ,where a nose-like structure is most favorable for oil/gas migration and accumulation. Based on the above work,a comprehensive evaluation of reservoir formation was carried out based on regional seal distribution,reservoir prediction and existing drilling records,to direct future exploration.
Carbonate rock is the major target horizon for Paleogene oil/gas exploration in the Tazhong area of the Tarim Basin. Study of the major factors controlling reservoir formation plays an important role in carbonate exploration. The complexity of reservoir forming in Tazhong block Ⅲ has restricted exploration,so analysis of carbonate reservoir deposition and later re-formation was carried out in terms of tectonic evolution to confirm that the high-energy facies controlled by faulted uplifting was the material basis for karstification. High-energy shoals and inner platform gentle shoals are widely developed in Tazhong block Ⅲ. The feather-shaped fractured zone and echelon faults in the NE strike-slip fault system are favorable areas for reservoir development. The paleostructures in the crucial period of hydrocarbon accumulation controlled the migration pathway for Paleogene oil/gas migration from north to south in Tazhong block Ⅲ,where a nose-like structure is most favorable for oil/gas migration and accumulation. Based on the above work,a comprehensive evaluation of reservoir formation was carried out based on regional seal distribution,reservoir prediction and existing drilling records,to direct future exploration.
引文
[1]翟光明，何文渊.塔里木盆地石油勘探实现突破的重要方向[J].石油学报，2004,25(1):1-7.[Zhai Guangming,He Wenyuan. An important petroleum exploration region in Tarim Basin[J]. Acta Petrolei Sinica,2004,25(1):1-7.]
[2]吕修祥，金之钧.碳酸盐岩油气田分布规律[J].石油学报，2000,21(3):8-12.[LüXiuxiang,Jin Zhijun. Distribution patterns of oil-gas fields in the carbonate rock[J]. Acta Petrolei Sinica,2000,21(3):8-12.]
[3]周新源，吕修祥，杨海军，等.塔中北斜坡走滑断裂对碳酸盐岩油气差异富集的影响[J].石油学报，2013,34(4):628-637.[Zhou Xinyuan,LüXiuxiang,Yang Haijun,et al. Effects of strike-slip faults on the differential enrichment of hydrocarbons in the northern slope of Tazhong area[J]. Acta Petrolei Sinica,2013,34(4):628-637.]
[4]马永生，蔡勋育，郭彤楼，等.四川盆地普光大型气田油气充注与富集成藏的主控因素[J].科学通报，2007,52（增刊1):149-155.[Ma Yongsheng,Cai Xunyu,Guo Tonglou,et al. The controlling factors of oil and gas charging and accumulation of Puguang gas field in the Sichuan Basin[J]. Chinese Science Bulletin,2007,52(Suppl. 1):149-155.]
[5]胡再元，孙东，胡圆圆，等.断裂系统对碳酸盐岩储层的控制作用：以塔里木盆地塔中Ⅲ区奥陶系为例[J].天然气地球科学，2015,26（增刊1):97-108.[Hu Zaiyuan,Sun Dong,Hu Yuanyuan,et al. The controlling effect of carbonate fault system on reservoirs:A case study in the 3rd block of Tazhong area[J]. Natural Gas Geoscience,2015,26(Suppl. 1):97-108.]
[6]贾承造，魏国齐.塔里木盆地构造特征与含油气性[J].科学通报，2002,47（增刊1):1-8.[Jia Chengzao,Wei Guoqi. Structural characteristics and petroliferous features of Tarim Basin[J]. Chinese Science Bulletin,2002,47(Suppl. 1):1-8.]
[7]李传新，贾承造，李本亮，等.塔里木盆地塔中低凸起北斜坡古生代断裂展布与构造演化[J].地质学报，2009,83(8):1065-1073.[Li Chuanxin,Jia Chengzao,Li Benliang,et al. Distribution and tectonic evolution of the Paleozoic fault system,the north slope of Tazhong uplift,Tarim Basin[J]. Acta Geologica Sinica,2009,83(8):1065-1073.]
[8]李本亮，管树巍，李传新，等.塔里木盆地塔中低凸起古构造演化与变形特征[J].地质论评，2009,55(4):522-530.[Li Benliang,Guan Shuwei,Li Chuanxin,et al. Paleo-tectonic evolution and deformation features of the lower uplift in the central Tarim Basin[J]. Geological Review, 2009, 55(4):522-530.]
[9]王福焕，王招明，韩剑发，等.塔里木盆地塔中地区碳酸盐岩油气富集的地质条件[J].天然气地球科学，2009,20(5):695-702.[Wang Fuhuan,Wang Zhaoming,Han Jianfa,et al. Geological conditions of oil and gas enrichment in carbonate reservoirs of Tazhong area,Tarim Basin[J]. Natural Gas Geoscience,2009,20(5):695-702.]
[10]杨海军，韩剑发，陈利新，等.塔中古隆起下古生界碳酸盐岩油气复式成藏特征及模式[J].石油与天然气地质，2007,28(6):784-790.[Yang Haijun,Han Jianfa,Chen Lixin,et al.Characteristics and patterns of complex hydrocarbon accumulation in the Lower Paleozoic carbonate rocks of the Tazhong palaeouplift[J]. Oil&Gas Geology,2007,28(6):784-790.]
[11]李素梅，庞雄奇，杨海军，等.塔里木盆地海相油气源与混源成藏模式[J].地球科学——中国地质大学学报，2010,35(4):663-673.[Li Sumei,Pang Xiongqi,Yang Haijun,et al. Generation,migration and accumulation model for the marine oils in the Tarim Basin[J]. Earth Science-Journal of China University of Geosciences,2010,35(4):663-673.]
[12]白忠凯，吕修祥，于红枫，等.塔中地区下古生界碳酸盐岩输导体系特征及成藏意义[J].地质科技情报，2011,30(5):60-68.[Bai Zhongkai,LüXiuxiang,Yu Hongfeng,et al. Characteristics and accumulation significance of the pathway systems in Lower Palaeozoic carbonate,Tazhong area[J]. Geological Science and Technology Information,2011,30(5):60-68.]
[13]吕修祥，金之钧，皮学军，等.塔里木盆地下古生界碳酸盐岩油气聚集与分布[J].中国科学（D辑）：地球科学，1999,29(4):358-361.[LüXiuxiang,Jin Zhijun,Pi Xuejun,et al. Hydrocarbon accumulation and distribution in Lower Paleozoic carbonates in Tarim Basin[J]. Science China(Seri. D):Earth Sciences,1999,29(4):358-361.]
[14]杨海军，邬光辉，韩剑发，等.塔里木盆地中央隆起带奥陶系碳酸盐岩台缘带油气富集特征[J].石油学报，2007,28(4):26-30.[Yang Haijun,Wu Guanghui,Han Jianfa,et al. Characteristics of hydrocarbon enrichment along the Ordovician carbonate platform margin in the central uplift of Tarim Basin[J]. Acta Petrolei Sinica,2007,28(4):26-30.]
[15]焦伟伟，吕修祥，周园园，等.塔里木盆地塔中地区奥陶系碳酸盐岩储层主控因素[J].石油与天然气地质，2011,32(2):199-206.[Jiao Weiwei,LüXiuxiang,Zhou Yuanyuan,et al.Main controlling factors of the Ordovician carbonate reservoirs in Tazhong area,the Tarim Basin[J]. Oil&Gas Geology,2011,32(2):199-206.]
[16]韩杰，江杰，潘文庆，等.塔中西部奥陶系桑塔木组底界灰岩段的识别及沉积学意义[J].天然气地球科学，2014,25(4):490-497.[Han Jie,Jiang Jie,Pan Wenqing,et al. Identification of limestone formation below Sangtamu Group of Ordovician and its sedimentary meaning in western Tazhong[J]. Natural Gas Geoscience,2014,25(4):490-497.]
[17]冯增昭，鲍志东，吴茂炳，等.塔里木地区奥陶纪岩相古地理[J].古地理学报，2007,9(5):447-460.[Feng Zengzhao,Bao Zhidong,Wu Maobing,et al. Lithofacies palaeogeography of the Ordovician in Tarim area[J]. Journal of Palaeogeography,2007,9(5):447-460.]
[18]孙东，杨丽莎，王宏斌，等.塔里木盆地哈拉哈塘地区走滑断裂体系对奥陶系海相碳酸盐岩储层的控制作用[J].天然气地球科学，2015,26（增刊1):80-87.[Sun Dong,Yang Lisha,Wang Hongbin,et al. Strike-slip fault system in Halahatang area of Tarim Basin and its control on reservoirs of Ordovician marine carbonate rock[J]. Natural Gas Geoscience,2015,26(Suppl. 1):80-87.]
[19]吕修祥，杨宁，周新源，等.塔里木盆地断裂活动对奥陶系碳酸盐岩储层的影响[J].中国科学（D辑）：地球科学，2008,38（增刊1):48-54.[LüXiuxiang,Yang Ning,Zhou Xinyuan,et al. Influence of Ordovician carbonate reservoir beds in Tarim Basin by faulting[J]. Science China(Seri. D):Earth Sciences,2008,38(Suppl. 1):48-54.]
[20]潘文庆，刘永福，Dickson J A D，等.塔里木盆地下古生界碳酸盐岩热液岩溶的特征及地质模型[J].沉积学报，2009,27(5):983-994.[Pan Wenqing,Liu Yongfu,Dickson J A D,et al.The geological model of hydrothermal activity in outcrop and the characteristics of carbonate hydrothermal karst of Lower Paleozoic in Tarim Basin[J]. Acta Sedimentologica Sinica,2009,27(5):983-994.]
[21]张仲培，王毅，云金表，等.塔中地区断裂不同演化阶段对油气聚集的控制[J].石油与天然气地质，2009,30(3):316-323,315.[Zhang Zhongpei,Wang Yi,Yun Jinbiao,et al. Control of faults at different evolution stages on hydrocarbon accumulation in Tazhong area,the Tarim Basin[J]. Oil&Gas Geology,2009,30(3):316-323,315.]
[22]李萌，汤良杰，漆立新，等.塔北隆起南坡差异构造演化及其对油气成藏的控制[J].天然气地球科学，2015,26(2):218-228.[Li Meng,Tang Liangjie,Qi Lixin,et al. Differential tectonic evolution and its controlling on hydrocarbon accumulation in the south slope of Tabei uplift[J]. Natural Gas Geoscience,2015,26(2):218-228.]
[23]朱光有，杨海军，朱永峰，等.塔里木盆地哈拉哈塘地区碳酸盐岩油气地质特征与富集成藏研究[J].岩石学报，2011,27(3):827-844.[Zhu Guangyou,Yang Haijun,Zhu Yongfeng,et al. Study on petroleum geological characteristics and accumulation of carbonate reservoirs in Hanilcatam area,Tarim Basin[J]. Acta Petrologica Sinica,2011,27(3):827-844.]
[24]苏劲，张水昌，杨海军，等.断裂系统对碳酸盐岩有效储层的控制及其成藏规律[J].石油学报，2010,31(2):196-203.[Su Jin,Zhang Shuichang,Yang Haijun,et al. Control of fault system to formation of effective carbonate reservoir and the rules of petroleum accumulation[J]. Acta Petrolei Sinica,2010,31(2):196-203.]
[25]张水昌，梁狄刚，黎茂稳，等.分子化石与塔里木盆地油源对比[J].科学通报，2002,47（增刊1):16-23.[Zhang Shuichang,Liang Digang,Li Maowen,et al. Molecular fossils and oilsource rock correlations in Tarim Basin,NW China[J]. Chinese Science Bulletin,2002,47(Suppl. 1):16-23.]
[26]张兴阳，张水昌，罗平，等.塔中地区晚燕山—喜马拉雅期油气调整与热液活动的关系[J].科学通报，2007,52（增刊1):192-198.[Zhang Xingyang,Zhang Shuichang,Luo Ping,et al. Late Yanshan-Himalayan hydrocarbon reservoir adjustment and hydrothermal fluid activity in the central Tarim Basin[J].Chinese Science Bulletin,2007,52(Suppl. 1):192-198.]
[27]陈利新，杨海军，邬光辉，等.塔中Ⅰ号坡折带奥陶系礁滩体油气藏的成藏特点[J].新疆石油地质，2008,29(3):327-330.[Chen Lixin,Yang Haijun,Wu Guanghui,et al. Characteristics of the Ordovician reef-shoal reservoir in Tazhong No. 1 slope-break zone,Tarim Basin[J]. Xinjiang Petroleum Geology,2008,29(3):327-330.]
[28]肖中尧，张水昌，赵孟军，等.简析塔中北斜坡A井志留系油气藏成藏期[J].沉积学报，1997,15(2):150-154.[Xiao Zhongyao,Zhang Shuichang,Zhao Mengjun,et al. A brief analysis on forming periods of Silurian pools in the Tazhong A Well[J]. Acta Sedimentologica Sinica, 1997, 15(2):150-154.]
[29]林青，王培荣，金晓辉，等.塔中北斜坡塔中45井奥陶系油藏成藏史浅析[J].石油勘探与开发，2002,29(3):5-7.[Lin Qing,Wang Peirong,Jin Xiaohui,et al. Reservoir-forming history of Ordovician reservoir at Well Tazhong 45 in the northern slope of Tazhong uplift[J]. Petroleum Exploration and Development,2002,29(3):5-7.]
[30] Song G Q,Chen H H. Quantitative evaluation of transporting efficiencies for hydrocarbon migration along different unconformities in a Cainozoic lacustrine basin:Examples from the Dongying Depression,Bohai Bay Basin,East China[J]. Journal of Geochemical Exploration,2009,101(1):97.
[31]孙东，潘建国，潘文庆，等.塔中地区碳酸盐岩溶洞储层体积定量化正演模拟[J].石油与天然气地质，2010,31(6):871-878,882.[Sun Dong,Pan Jianguo,Pan Wenqing,et al. Quantitative forward modelling of cavity volume in carbonate reservoirs in Tazhong area[J]. Oil&Gas Geology,2010,31(6):871-878,882.]
[32]孙东，潘建国，雍学善，等.碳酸盐岩储层垂向长串珠形成机制[J].石油地球物理勘探，2010,45（增刊1):101-104.[Sun Dong,Pan Jianguo,Yong Xueshan,et al. Formation mechanism of vertical"long string beads"in carbonate reservoir[J].Oil Geophysical Prospecting,2010,45(Suppl. 1):101-104.]
[33] Yao Y,Xi X. Reflected wavefield in random media:a review[J]. Journal of Geophysics and Engineering,2004,1(2):147-152.
[34]吴永国，贺振华，黄德济.串珠状溶洞模型介质波动方程正演与偏移[J].地球物理学进展，2008,23(2):539-544.[Wu Yongguo,He Zhenhua,Huang Deji. Wave equation forward modeling and migration for beads-shaped corroded cave model[J]. Progress in Geophysics,2008,23(2):539-544.]
[2]吕修祥，金之钧.碳酸盐岩油气田分布规律[J].石油学报，2000,21(3):8-12.[LüXiuxiang,Jin Zhijun. Distribution patterns of oil-gas fields in the carbonate rock[J]. Acta Petrolei Sinica,2000,21(3):8-12.]
[3]周新源，吕修祥，杨海军，等.塔中北斜坡走滑断裂对碳酸盐岩油气差异富集的影响[J].石油学报，2013,34(4):628-637.[Zhou Xinyuan,LüXiuxiang,Yang Haijun,et al. Effects of strike-slip faults on the differential enrichment of hydrocarbons in the northern slope of Tazhong area[J]. Acta Petrolei Sinica,2013,34(4):628-637.]
[4]马永生，蔡勋育，郭彤楼，等.四川盆地普光大型气田油气充注与富集成藏的主控因素[J].科学通报，2007,52（增刊1):149-155.[Ma Yongsheng,Cai Xunyu,Guo Tonglou,et al. The controlling factors of oil and gas charging and accumulation of Puguang gas field in the Sichuan Basin[J]. Chinese Science Bulletin,2007,52(Suppl. 1):149-155.]
[5]胡再元，孙东，胡圆圆，等.断裂系统对碳酸盐岩储层的控制作用：以塔里木盆地塔中Ⅲ区奥陶系为例[J].天然气地球科学，2015,26（增刊1):97-108.[Hu Zaiyuan,Sun Dong,Hu Yuanyuan,et al. The controlling effect of carbonate fault system on reservoirs:A case study in the 3rd block of Tazhong area[J]. Natural Gas Geoscience,2015,26(Suppl. 1):97-108.]
[6]贾承造，魏国齐.塔里木盆地构造特征与含油气性[J].科学通报，2002,47（增刊1):1-8.[Jia Chengzao,Wei Guoqi. Structural characteristics and petroliferous features of Tarim Basin[J]. Chinese Science Bulletin,2002,47(Suppl. 1):1-8.]
[7]李传新，贾承造，李本亮，等.塔里木盆地塔中低凸起北斜坡古生代断裂展布与构造演化[J].地质学报，2009,83(8):1065-1073.[Li Chuanxin,Jia Chengzao,Li Benliang,et al. Distribution and tectonic evolution of the Paleozoic fault system,the north slope of Tazhong uplift,Tarim Basin[J]. Acta Geologica Sinica,2009,83(8):1065-1073.]
[8]李本亮，管树巍，李传新，等.塔里木盆地塔中低凸起古构造演化与变形特征[J].地质论评，2009,55(4):522-530.[Li Benliang,Guan Shuwei,Li Chuanxin,et al. Paleo-tectonic evolution and deformation features of the lower uplift in the central Tarim Basin[J]. Geological Review, 2009, 55(4):522-530.]
[9]王福焕，王招明，韩剑发，等.塔里木盆地塔中地区碳酸盐岩油气富集的地质条件[J].天然气地球科学，2009,20(5):695-702.[Wang Fuhuan,Wang Zhaoming,Han Jianfa,et al. Geological conditions of oil and gas enrichment in carbonate reservoirs of Tazhong area,Tarim Basin[J]. Natural Gas Geoscience,2009,20(5):695-702.]
[10]杨海军，韩剑发，陈利新，等.塔中古隆起下古生界碳酸盐岩油气复式成藏特征及模式[J].石油与天然气地质，2007,28(6):784-790.[Yang Haijun,Han Jianfa,Chen Lixin,et al.Characteristics and patterns of complex hydrocarbon accumulation in the Lower Paleozoic carbonate rocks of the Tazhong palaeouplift[J]. Oil&Gas Geology,2007,28(6):784-790.]
[11]李素梅，庞雄奇，杨海军，等.塔里木盆地海相油气源与混源成藏模式[J].地球科学——中国地质大学学报，2010,35(4):663-673.[Li Sumei,Pang Xiongqi,Yang Haijun,et al. Generation,migration and accumulation model for the marine oils in the Tarim Basin[J]. Earth Science-Journal of China University of Geosciences,2010,35(4):663-673.]
[12]白忠凯，吕修祥，于红枫，等.塔中地区下古生界碳酸盐岩输导体系特征及成藏意义[J].地质科技情报，2011,30(5):60-68.[Bai Zhongkai,LüXiuxiang,Yu Hongfeng,et al. Characteristics and accumulation significance of the pathway systems in Lower Palaeozoic carbonate,Tazhong area[J]. Geological Science and Technology Information,2011,30(5):60-68.]
[13]吕修祥，金之钧，皮学军，等.塔里木盆地下古生界碳酸盐岩油气聚集与分布[J].中国科学（D辑）：地球科学，1999,29(4):358-361.[LüXiuxiang,Jin Zhijun,Pi Xuejun,et al. Hydrocarbon accumulation and distribution in Lower Paleozoic carbonates in Tarim Basin[J]. Science China(Seri. D):Earth Sciences,1999,29(4):358-361.]
[14]杨海军，邬光辉，韩剑发，等.塔里木盆地中央隆起带奥陶系碳酸盐岩台缘带油气富集特征[J].石油学报，2007,28(4):26-30.[Yang Haijun,Wu Guanghui,Han Jianfa,et al. Characteristics of hydrocarbon enrichment along the Ordovician carbonate platform margin in the central uplift of Tarim Basin[J]. Acta Petrolei Sinica,2007,28(4):26-30.]
[15]焦伟伟，吕修祥，周园园，等.塔里木盆地塔中地区奥陶系碳酸盐岩储层主控因素[J].石油与天然气地质，2011,32(2):199-206.[Jiao Weiwei,LüXiuxiang,Zhou Yuanyuan,et al.Main controlling factors of the Ordovician carbonate reservoirs in Tazhong area,the Tarim Basin[J]. Oil&Gas Geology,2011,32(2):199-206.]
[16]韩杰，江杰，潘文庆，等.塔中西部奥陶系桑塔木组底界灰岩段的识别及沉积学意义[J].天然气地球科学，2014,25(4):490-497.[Han Jie,Jiang Jie,Pan Wenqing,et al. Identification of limestone formation below Sangtamu Group of Ordovician and its sedimentary meaning in western Tazhong[J]. Natural Gas Geoscience,2014,25(4):490-497.]
[17]冯增昭，鲍志东，吴茂炳，等.塔里木地区奥陶纪岩相古地理[J].古地理学报，2007,9(5):447-460.[Feng Zengzhao,Bao Zhidong,Wu Maobing,et al. Lithofacies palaeogeography of the Ordovician in Tarim area[J]. Journal of Palaeogeography,2007,9(5):447-460.]
[18]孙东，杨丽莎，王宏斌，等.塔里木盆地哈拉哈塘地区走滑断裂体系对奥陶系海相碳酸盐岩储层的控制作用[J].天然气地球科学，2015,26（增刊1):80-87.[Sun Dong,Yang Lisha,Wang Hongbin,et al. Strike-slip fault system in Halahatang area of Tarim Basin and its control on reservoirs of Ordovician marine carbonate rock[J]. Natural Gas Geoscience,2015,26(Suppl. 1):80-87.]
[19]吕修祥，杨宁，周新源，等.塔里木盆地断裂活动对奥陶系碳酸盐岩储层的影响[J].中国科学（D辑）：地球科学，2008,38（增刊1):48-54.[LüXiuxiang,Yang Ning,Zhou Xinyuan,et al. Influence of Ordovician carbonate reservoir beds in Tarim Basin by faulting[J]. Science China(Seri. D):Earth Sciences,2008,38(Suppl. 1):48-54.]
[20]潘文庆，刘永福，Dickson J A D，等.塔里木盆地下古生界碳酸盐岩热液岩溶的特征及地质模型[J].沉积学报，2009,27(5):983-994.[Pan Wenqing,Liu Yongfu,Dickson J A D,et al.The geological model of hydrothermal activity in outcrop and the characteristics of carbonate hydrothermal karst of Lower Paleozoic in Tarim Basin[J]. Acta Sedimentologica Sinica,2009,27(5):983-994.]
[21]张仲培，王毅，云金表，等.塔中地区断裂不同演化阶段对油气聚集的控制[J].石油与天然气地质，2009,30(3):316-323,315.[Zhang Zhongpei,Wang Yi,Yun Jinbiao,et al. Control of faults at different evolution stages on hydrocarbon accumulation in Tazhong area,the Tarim Basin[J]. Oil&Gas Geology,2009,30(3):316-323,315.]
[22]李萌，汤良杰，漆立新，等.塔北隆起南坡差异构造演化及其对油气成藏的控制[J].天然气地球科学，2015,26(2):218-228.[Li Meng,Tang Liangjie,Qi Lixin,et al. Differential tectonic evolution and its controlling on hydrocarbon accumulation in the south slope of Tabei uplift[J]. Natural Gas Geoscience,2015,26(2):218-228.]
[23]朱光有，杨海军，朱永峰，等.塔里木盆地哈拉哈塘地区碳酸盐岩油气地质特征与富集成藏研究[J].岩石学报，2011,27(3):827-844.[Zhu Guangyou,Yang Haijun,Zhu Yongfeng,et al. Study on petroleum geological characteristics and accumulation of carbonate reservoirs in Hanilcatam area,Tarim Basin[J]. Acta Petrologica Sinica,2011,27(3):827-844.]
[24]苏劲，张水昌，杨海军，等.断裂系统对碳酸盐岩有效储层的控制及其成藏规律[J].石油学报，2010,31(2):196-203.[Su Jin,Zhang Shuichang,Yang Haijun,et al. Control of fault system to formation of effective carbonate reservoir and the rules of petroleum accumulation[J]. Acta Petrolei Sinica,2010,31(2):196-203.]
[25]张水昌，梁狄刚，黎茂稳，等.分子化石与塔里木盆地油源对比[J].科学通报，2002,47（增刊1):16-23.[Zhang Shuichang,Liang Digang,Li Maowen,et al. Molecular fossils and oilsource rock correlations in Tarim Basin,NW China[J]. Chinese Science Bulletin,2002,47(Suppl. 1):16-23.]
[26]张兴阳，张水昌，罗平，等.塔中地区晚燕山—喜马拉雅期油气调整与热液活动的关系[J].科学通报，2007,52（增刊1):192-198.[Zhang Xingyang,Zhang Shuichang,Luo Ping,et al. Late Yanshan-Himalayan hydrocarbon reservoir adjustment and hydrothermal fluid activity in the central Tarim Basin[J].Chinese Science Bulletin,2007,52(Suppl. 1):192-198.]
[27]陈利新，杨海军，邬光辉，等.塔中Ⅰ号坡折带奥陶系礁滩体油气藏的成藏特点[J].新疆石油地质，2008,29(3):327-330.[Chen Lixin,Yang Haijun,Wu Guanghui,et al. Characteristics of the Ordovician reef-shoal reservoir in Tazhong No. 1 slope-break zone,Tarim Basin[J]. Xinjiang Petroleum Geology,2008,29(3):327-330.]
[28]肖中尧，张水昌，赵孟军，等.简析塔中北斜坡A井志留系油气藏成藏期[J].沉积学报，1997,15(2):150-154.[Xiao Zhongyao,Zhang Shuichang,Zhao Mengjun,et al. A brief analysis on forming periods of Silurian pools in the Tazhong A Well[J]. Acta Sedimentologica Sinica, 1997, 15(2):150-154.]
[29]林青，王培荣，金晓辉，等.塔中北斜坡塔中45井奥陶系油藏成藏史浅析[J].石油勘探与开发，2002,29(3):5-7.[Lin Qing,Wang Peirong,Jin Xiaohui,et al. Reservoir-forming history of Ordovician reservoir at Well Tazhong 45 in the northern slope of Tazhong uplift[J]. Petroleum Exploration and Development,2002,29(3):5-7.]
[30] Song G Q,Chen H H. Quantitative evaluation of transporting efficiencies for hydrocarbon migration along different unconformities in a Cainozoic lacustrine basin:Examples from the Dongying Depression,Bohai Bay Basin,East China[J]. Journal of Geochemical Exploration,2009,101(1):97.
[31]孙东，潘建国，潘文庆，等.塔中地区碳酸盐岩溶洞储层体积定量化正演模拟[J].石油与天然气地质，2010,31(6):871-878,882.[Sun Dong,Pan Jianguo,Pan Wenqing,et al. Quantitative forward modelling of cavity volume in carbonate reservoirs in Tazhong area[J]. Oil&Gas Geology,2010,31(6):871-878,882.]
[32]孙东，潘建国，雍学善，等.碳酸盐岩储层垂向长串珠形成机制[J].石油地球物理勘探，2010,45（增刊1):101-104.[Sun Dong,Pan Jianguo,Yong Xueshan,et al. Formation mechanism of vertical"long string beads"in carbonate reservoir[J].Oil Geophysical Prospecting,2010,45(Suppl. 1):101-104.]
[33] Yao Y,Xi X. Reflected wavefield in random media:a review[J]. Journal of Geophysics and Engineering,2004,1(2):147-152.
[34]吴永国，贺振华，黄德济.串珠状溶洞模型介质波动方程正演与偏移[J].地球物理学进展，2008,23(2):539-544.[Wu Yongguo,He Zhenhua,Huang Deji. Wave equation forward modeling and migration for beads-shaped corroded cave model[J]. Progress in Geophysics,2008,23(2):539-544.]
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