塔里木盆地石炭系烃源岩成熟演化研究
|
摘要
尽管塔里木盆地石炭系富含有机质且已发现其生成的原油,但关于石炭系烃源岩热演化研究却很薄弱。根据基础地质资料、古地温梯度和实测镜质体反射率数据,本文定量模拟了塔里木盆地6口典型井的石炭系烃源岩热演化史和这套烃源岩底界、顶界在二叠纪末期、三叠纪末期、白垩纪末期及现今成熟度的平面分布规律。塔北隆起南部、塔西南坳陷和阿瓦提凹陷在石炭—二叠纪作为沉降中心接受了巨厚的沉积物,造成这些地区石炭系烃源岩底界成熟度在二叠纪末期达到0.9%~1.3%(中—高成熟),顶界为0.5%~0.9%(低—中成熟),成为有利生油区。中生代时期,塔里木盆地中、东部长期处于沉降状态,石炭系烃源岩处于成熟演化阶段。白垩纪末期,塔中低凸起和满加尔凹陷的石炭系底界成熟度为0.7%~0.9%(中成熟),顶界为0.5%~0.7%(低成熟);而塘古孜巴斯坳陷底界成熟度为0.9%~1_1%(中—高成熟),顶界为0.7%~0.9%(中成熟)。受羌塘地体、拉萨地体、印度板块分别与欧亚板块南缘碰撞远程效应的影响,塔西南坳陷和巴楚隆起在中生代一直处于隆升剥蚀状态,烃源岩热演化进入停滞状态。新生代以来,塔西南坳陷和阿瓦提凹陷演化为前陆盆地,再次接受了巨厚沉积物,致使石炭系烃源岩快速成熟演化,底一顶界成熟度现今已超过2.0%,进入干气阶段。满加尔凹陷石炭系烃源岩自石炭纪至今一直处于成熟演化阶段,现今达到最大,为0.8%~1.0%。另外,热史研究表明塔西南坳陷和阿瓦提凹陷石炭系烃源岩具有二次生烃潜力。本研究不仅丰富了塔里木盆地石炭系烃源岩热史研究成果,而且对油气勘探与开发具有重要的指导意义。
For the Carboniferous of the Tarim Basin,although it is rich in source rocks and the crude oil which generated were found,the studies on its thermal evolution are very few.Based on the geological data,paleo-geothermal gradient and measured vitrinite reflectance data,we simulated the thermal evolution of the Carboniferous source rocks(CSR) of 6 typical wells in the Tarim Basin and rebuilt quantitatively the maturity distribution characteristic of the base and top of the CSR in the end of Permian,the end of Triassic,the end of Cretaceous and presentday,respectively.As the deposition centers,the massive sediments were deposited in the southern Tabei uplift,Southwest depression and Awati depression during the Carboniferous and the Permian,which caused the maturity evolution of the CSR in these areas.In the end of Permian,the maturity of the base of the CSR in the southern Tabei uplift,Southwest depression and Awati depression reached to 0.9%~ 1.3%(middle-high maturity) and the top was just 0.5%~0.9%(low-middle maturity),which indicated that these areas were favorable to generate oil in the Permian.The CSR in the central-eastern Tarim Basin always stayed in the maturity evolution stage due to the long-term deposition in the Mesozoic.The maturity of the base of the CSR in the Tazhong low-uplift and Manjiaer depression was 0.7%~ 0.9%(middle maturity) and their top was 0.5%~0.7%(low maturity) in the end of Cretaceous,while the base of the Tangguzibasi depression was 0.9%~ 1.1%(middle-high maturity) and its top was0.7%~0.9%(middle maturity).The Southwest depression and Bachu uplift experienced uplift and erosion during the Mesozoic and the maturity of their SCR stopped evolution due to the distant effect from the collision among the Qiangtang block,Lhasa block and Indian plate with the southern margin of the Eurasia continent.Since the Cenozoic,the Southwest depression and Awati depression developed as the foreland basins and received massive sediments again,which caused the rapid evolution of the maturity of the SCR.The maturity of the base and top of the SCR in the Southwest depression and Awati depression is larger than 2.0%now and stays in the dry-gas stage.The maturity of the SCR in the Manjiaer depression always stayed in evolving since the Carboniferous and reach to the maximum with 0.8%~ 1.0%now.In addition,the potential area of secondary hydrocarbon generation for the SCR were the Southwest depression and Awati depression.This study not only enriches the research on the thermal histories of the SCR,but also provides guidance for the oil and gas exploration and exploitation in the Tarim Basin.
For the Carboniferous of the Tarim Basin,although it is rich in source rocks and the crude oil which generated were found,the studies on its thermal evolution are very few.Based on the geological data,paleo-geothermal gradient and measured vitrinite reflectance data,we simulated the thermal evolution of the Carboniferous source rocks(CSR) of 6 typical wells in the Tarim Basin and rebuilt quantitatively the maturity distribution characteristic of the base and top of the CSR in the end of Permian,the end of Triassic,the end of Cretaceous and presentday,respectively.As the deposition centers,the massive sediments were deposited in the southern Tabei uplift,Southwest depression and Awati depression during the Carboniferous and the Permian,which caused the maturity evolution of the CSR in these areas.In the end of Permian,the maturity of the base of the CSR in the southern Tabei uplift,Southwest depression and Awati depression reached to 0.9%~ 1.3%(middle-high maturity) and the top was just 0.5%~0.9%(low-middle maturity),which indicated that these areas were favorable to generate oil in the Permian.The CSR in the central-eastern Tarim Basin always stayed in the maturity evolution stage due to the long-term deposition in the Mesozoic.The maturity of the base of the CSR in the Tazhong low-uplift and Manjiaer depression was 0.7%~ 0.9%(middle maturity) and their top was 0.5%~0.7%(low maturity) in the end of Cretaceous,while the base of the Tangguzibasi depression was 0.9%~ 1.1%(middle-high maturity) and its top was0.7%~0.9%(middle maturity).The Southwest depression and Bachu uplift experienced uplift and erosion during the Mesozoic and the maturity of their SCR stopped evolution due to the distant effect from the collision among the Qiangtang block,Lhasa block and Indian plate with the southern margin of the Eurasia continent.Since the Cenozoic,the Southwest depression and Awati depression developed as the foreland basins and received massive sediments again,which caused the rapid evolution of the maturity of the SCR.The maturity of the base and top of the SCR in the Southwest depression and Awati depression is larger than 2.0%now and stays in the dry-gas stage.The maturity of the SCR in the Manjiaer depression always stayed in evolving since the Carboniferous and reach to the maximum with 0.8%~ 1.0%now.In addition,the potential area of secondary hydrocarbon generation for the SCR were the Southwest depression and Awati depression.This study not only enriches the research on the thermal histories of the SCR,but also provides guidance for the oil and gas exploration and exploitation in the Tarim Basin.
引文
蔡希源.2007.塔里木盆地大中型油气田成控因素与展布规律.石油与天然气地质,28(6):693—702.Cai Xiyuan.2007.Main factors controlling hydrocarbon accumulation of middle-and large-sized oil and gas fields and their distribution rules in the Tarim Basin.Oil&Gas Geology,28(6):693—702.
陈荣林.1987.塔里木盆地三叠—侏罗系沉积及其油气远景.石油实验地质,9(3):251—258.Chen Ronglin.1987.The prospects for oil and gas,and the sedimentary sequences from Triassic to Jurassic in Tarim Basin.Experimental Petroleum Geology,9(3):251—258.
德勒达尔.1996.塔里木盆地西部石炭—二叠纪沉积体系及沉积相.新疆石油地质,17(4):350—357.Del Dar.1996.Sedimentary system and facies of Carboniferous-Permian in western Tarim Basin.Xinjiang Petroleum Geology,17(4):350—357.
段毅,周世新.1999.塔里木盆地石炭系烃源岩热模拟实验地球化学研究——I.气态和液态产物的产率及演化特征.沉积学报,17(增刊):832—835.Duan Yi and Zhou Shixin,1999.Geochemical study of thermal simulation of Carboniferous source rock in the Tarim Basin——I.Yield of gaseous and liquid products and the evolution characteristics.Acta Sedimentologica Sinica,17(suppl.):832—835.
冯昌格,刘绍文,王良书等.2009.塔里木盆地现今地热特征.地球物理学报,52(11):2752—2762.Feng Changge,Liu Shaowen,Wang Liangshu et al.2009.Present-day geothermal regime in Tarim Basin,Northwest China.Chinese Journal of Geophysics,52(11):2752—2762.
傅玮东,王健,刘绍民.2003.塔里木油田地区地表温度分布规律的研究.干旱区资源与环境,17(6):99—102.Fu Weidong,Wang Jian and Liu Shaomin.2003.Studies on the distribution rule of ground temperatures in Tarim oilfield.Journal of Arid and Resources and Environment,17(6):99—102.
郭原草.2009.塔里木盆地石炭系层序地层学研究(硕士学位论文).长沙:中南大学.1—72.Guo Yuancao.2009.Sequence Stratigraphy of Carboniferous in Tarim Basin(Master Thesis).Changsha:Central South University.1—72.
何登发,贾承造,李德生等.2005.塔里木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.Oil&Gas Geology,26(1):64—77.
何登发,李德生,何金有等.2013.塔里木盆地库车坳陷和西南坳陷油气地质特征类比及勘探启示.石油学报,34(2):201—218.He Dengfa,Li Desheng,He Jinyou et al.2013.Comparison in petroleum geology between Kuqa depression and southwest depression in Tarim Basin and its exploration significance.Acta Petrolei Sinica,34(2):201—218.
胡望水,陈毓遂,肖安成等.1997.塔西南坳陷构造演化与含油气系统.石油勘探与开发,24(1):14—17.Hu Wangshui,Chen Yusui,Xiao Ancheng et al.1997.Tectonic evolution and petroleum system in the southwest depression of Tarim Basin.Petroleum Exploration and Development,24(1):14—17.
贾承造.1997.中国塔里木盆地构造特征与油气.北京:石油工业出版社.1—420.Jia Chengzao.1997.Tectonics Characteristics of the Tarim Basin in China and Its Oil-Gas Resources.Beijing:Petroleum Industry Press.1—420.
金之钧,王清晨.2007.中国典型叠合盆地油气形成富集与分布预测.北京:科学出版社.1—265.Jin Zhijun and Wang Qingchen.2007.Formation,Accumulation and Distribution Prediction of Oil-Gas Resources in the Typical Superimposed Basins,China.Beijing:Science Press.1—265.
刘生国,薛天庆,刘学锋.2000.塔里木盆地石炭—第四纪构造演化与地层组合特征.西安科技学院学报,20(2):128—130.Liu Shengguo,Xue Tianqing and Liu Xuefeng.2000.The Carboniferous-Quaternary tectonic evolution and stratigraphic assemblages characteristics of Tarim Basin.Journal ofXi'an University of Science&Technology,20(2):128—130.
刘亚雷,胡秀芳,王道轩等.2012.塔里木盆地三叠纪岩相古地理特征.断块油气田,19(6):696—700.Liu Yalei,Hu Xiufang,Wang Daoxuan et al.2012.Characteristics of Triassic lithofacies palaeogeography in Tarim Basin.Fault-Block Oil&Gas Field,19(6):696—700.
潘长春,周中毅,范善发等.1996.塔里木盆地热历史.矿物岩石地球化学通报,15(3):150—152.Pan Changchun,Zhou Zhongyi,Fan Shanfa et al.1996.Thermal history of Tarim Basin.Bulletin of Mineralogy,Petrology and Geochemistry,15(3):150—152.
邱楠生,胡圣标,何丽娟.2004.沉积盆地热体制研究的理论与应用.北京:石油工业出版社.122—132.Qiu Nansheng,Hu Shengbiao and He Lijuan.2004.Theory and Application of Thermal Regime in Sedimentary Basins.Beijing:Petroleum Industry Press.122—132.
汤良杰.1994.塔里木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.
唐武,王英民,张雷等.2013.塔里木盆地三叠纪前缘隆起迁移演化规律.古地理学报,15(2):219—230.Tang Wu,Wang Yingmin,Zhang Lei et al.2013.Forebulge migration and evolution of the Triassic in Tarim Basin.Journal of Palaeogeography,15(2):219—230.
田作基.2006.塔北前陆盆她与南天山造山带的耦合关系及油气分布特征.石油地质,11(4):16—20.Tian Zuoji.2006.Coupling relation between Tabei foreland basin and Nantianshan orogenic belt and their oil-gas distribution feature.Petroleum Geology,11(4):16—20.
王飞宇,张水昌,张宝民等.2003.塔里木盆地寒武系海相烃源岩有机成熟度及演化史.地球化学,32(5):461—468.Wang Feiyu,Zhang Shuichang,Zhang Baomin et al.2003.Maturity and its history of Cambrian marine source rocks in the Tarim Basin.Geochimica,32(5):461—468.
萧德铭,冯子辉.1999.塔里木盆地大庆区块烃源岩演化史与油气成藏期研究.石油实验地质,21(1):28—33.Xiao Deming and Feng Zihui.1999.Study on the evolutionary history of source rock and the pool-forming periods of hydrocarbon in the Daqing block of the Tarim Basin.Experimental Petroleum Geology,21(1):28—33.
辛艳朋,邱楠生,李慧莉.2011.塔里木盆地下古生界烃源岩二次生烃范围研究.地球物理学报,s4(7):1863--1873.Xin Yanpeng,Qiu Nansheng and Li Huili.2011.The range of secondary hydrocarbon generation of Lower Palaeozoic source rock in Tarim Basin.Chinese Journal of Geophysics,54(7):1863^-1873.
邢卫新,汤达祯,马新海等.2007.塔里木盆地东北缘孔雀河地区烃源岩演化特征及成藏条件研究.天然气地球科学,18(1):57—61.Xing Wenxin,Tang Dazhen,Ma Xinhai et al.2007.Thermal evolution characteristics of hydrocarbon source rocks and pool forming conditions in the Kongque River area,northeastern fringe of Tarim Basin.Natural Gas Geoscience,18(1):57—61.
许杰.2009.塔里木盆地上泥盆统—石炭系层序地层学研究(博士学位论文).长沙:中南大学.1—222.Xu Jie.2009.Sequence Stratigrapy of Upper Devonian-Carboniferous in Tarim Basin(PhD Thesis).Changsha:Central South University.1—222.
许效松,刘宝珺,牟传龙等.2004.中国中西部海相盆地分析与油气资源.北京:地质出版社.47—55.Xu Xiaosong,Liu Baojun,Mou Chuanlong et al.2004.The Analysis of Marine Basins in Central and Western China and Its Hydrocarbon Resources.Beijing:Geological Publishing House.47-—55.
张斌,赵莆,张水昌等.2007.塔里木盆地和四川盆地海相烃源岩成烃演化模式探讨.科学通报,52(增刊):108—114.Zhang Bin,Zhao Zhe,Zhang Shuichang et al.2007.Discussion on marine source rooks thermal evoluement patterns in the Tarim Basin and Sichuan Basin,West China.Chinese Science Bulletin,52(suppl.):141—149.
张光亚,赵文智,王红军等.2007.塔里木盆地多旋回构造演化与复合含油气系统.石油与天然气地质,28(5):653—663.Zhang Guangya,Zhao Wenzhi,Wang Hongjun et al.2007.Multicycle tectonic evolution and composite petroleum systems in the Tarim Basin.Oil&Gas Geology,28(5):653—663.
张水昌,梁狄刚,张宝民等.2004a.塔里木盆地海相油气的生成.北京:石油工业出版社.1—200.Zhang Shuichang,Liang Digang,Zhang Baoming et al.2004.Marine Hydrocarbon Generation in the Tarim Basin.Beijing:Petroleum Industry Press.1—200.
张水昌,赵文智,王飞宇等.2004b.塔里木盆地东部地区古生界原油裂解气成藏历史分析——以荚南2气藏为例.天然气地球科学,15(5):441—451.Zhang Shuichang,Zhao Wenzhi,Wang Feiyu et al.2004.Paleozoic oil cracking gas accumulation history from eastern part of the Tarim Basin——A case study of the YN2 gas reservoir.Natural Gas Geoscience,15(5):441—451.
赵靖舟,李启明.2002.塔里术盆地克拉通区海相油气成藏期与成藏史.科学通报,47(增刊):116—121.Zhao Jingzhou and Li Qiming.2002.Timing and history of marine hydrocarbon accumulation in Tarim Craton.Chinese Science Bulletin,47(suppl.):120—127.
赵靖舟,李启明.2004.塔里木盆地油气藏形成与分布规律.北京:石油工业出版社.13—14.Zhao Jingzhou and Li Qiming.2004.Formation and Distribution of the Oil and Gas Reservoirs in the Tarim Basin.Beijing:Petroleum Industry Press.13—14.
朱如凯,罗平,罗忠.2002.塔里木盆地晚泥盆世及石炭纪岩相古地理.古地理学报,4(1):13—24.Zhu Rukai,Luo Ping and Luo Zhong.2002.Lithofacies palaeo-geography of the Late Devonian and Carboniferous in Tarim Basin.Journal of Palaeogeography,4(1):13—24.
Chen J S,Huang B C and Sun L S.2010.New constraints to the onset of the India-Asia collision:Paleomagnetic reconnaissance on the Linzizong Group in the Lhasa Block,China.Tectonophysics,489(1—4):189—209.
Kapp P,Yin A,Manning C E et al.2000.Blueschist-bearing metamorphic core complexes in the Qiangtang Block reveal deep crustal structure of northern Tibet.Geology,28(1):19—22.
Li M J,Wang T G,Chen J F et al.2010.Paleo-heat flow evolution of the Tabei uplift in Tarim Basin,Northwest China.Journal of Asian Earth Sciences,37(1):52—66.
Qiu N S,Chang J,Zuo Y H et al.2012.Thermal evolution and maturation of Lower Paleozoic source rocks in the Tarim Basin,Northwest China.AAPG Bulletin,96(5):789—821.
Robinson A C,Yin A,Manning C E et al.2004.Tectonic evolution of the northeastern Pamir:Constraints from the northern portion of the Cenozoic Kongur Shan extensional system,western China.GSA Bulletin,116(7—8):953—973.
Sobel E R.1999.Basin analysis of the Jurassic-Lower Cretaceous Southwest Tarim Basin,Northwest China.GSA Bulletin,111(5):709—724.
Vandenbroucke M,Behar F and Rudkiewicz J L.1999.Kinetic modelling of petroleum formation and cracking-Implications from the high pressure/high temperature Elgin Field(UK,North Sea).Organic Geochemistry,30(9):1105—1125.
Yin A and Harrison T M.2000.Geologic evolution of the Himalayan-Tibetan orogen.Annual Review of Earth and Planetary Sciences,28:211—280.
Zhang Q,Huang H,Zheng L et al.2007.Secondary hydrocarbon generation potential from heavy oil,oil sand and solid bitumen during the artificial maturation.Organic Geochemistry,38(12):2024—2035.
Zhu D C,Zhao Z D,Niu Y L et al.2013.The origin and pre-Cenozoic evolution of the Tibetan Plateau.Gondwana Research,23(4):1429—1454.
①金之钧等.2003.塔里木盆地台盆区有效烃源及油气勘探方向.中石化西指研究报告.
②谢觉新,周中毅,潘长春等.1994.塔里木盆地古地温、热演化史及油气评价.“八五”国家重点科技攻关项目“塔里木盆地油气资源”成果报告.
③解启来,周中毅,施继锡.1998.塔里木盆地生油岩成熟度确定及成烃演化史研究.“九五”国家重点攻关项目“塔里木盆地石油天然气勘探”成果报告.
④张水昌,王飞宇,张俊等.2000.塔里木盆地油源对比、烃源岩生烃史及油气藏形成史.“九五”国家重点攻关项目“塔里木盆地石油天然气勘探(二期)”成果报告.
⑤胡德庆,柳德全.2003.塔里木盆地构造演化史与构造控油特征研究.中石化西指立项报告.
陈荣林.1987.塔里木盆地三叠—侏罗系沉积及其油气远景.石油实验地质,9(3):251—258.Chen Ronglin.1987.The prospects for oil and gas,and the sedimentary sequences from Triassic to Jurassic in Tarim Basin.Experimental Petroleum Geology,9(3):251—258.
德勒达尔.1996.塔里木盆地西部石炭—二叠纪沉积体系及沉积相.新疆石油地质,17(4):350—357.Del Dar.1996.Sedimentary system and facies of Carboniferous-Permian in western Tarim Basin.Xinjiang Petroleum Geology,17(4):350—357.
段毅,周世新.1999.塔里木盆地石炭系烃源岩热模拟实验地球化学研究——I.气态和液态产物的产率及演化特征.沉积学报,17(增刊):832—835.Duan Yi and Zhou Shixin,1999.Geochemical study of thermal simulation of Carboniferous source rock in the Tarim Basin——I.Yield of gaseous and liquid products and the evolution characteristics.Acta Sedimentologica Sinica,17(suppl.):832—835.
冯昌格,刘绍文,王良书等.2009.塔里木盆地现今地热特征.地球物理学报,52(11):2752—2762.Feng Changge,Liu Shaowen,Wang Liangshu et al.2009.Present-day geothermal regime in Tarim Basin,Northwest China.Chinese Journal of Geophysics,52(11):2752—2762.
傅玮东,王健,刘绍民.2003.塔里木油田地区地表温度分布规律的研究.干旱区资源与环境,17(6):99—102.Fu Weidong,Wang Jian and Liu Shaomin.2003.Studies on the distribution rule of ground temperatures in Tarim oilfield.Journal of Arid and Resources and Environment,17(6):99—102.
郭原草.2009.塔里木盆地石炭系层序地层学研究(硕士学位论文).长沙:中南大学.1—72.Guo Yuancao.2009.Sequence Stratigraphy of Carboniferous in Tarim Basin(Master Thesis).Changsha:Central South University.1—72.
何登发,贾承造,李德生等.2005.塔里木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.Oil&Gas Geology,26(1):64—77.
何登发,李德生,何金有等.2013.塔里木盆地库车坳陷和西南坳陷油气地质特征类比及勘探启示.石油学报,34(2):201—218.He Dengfa,Li Desheng,He Jinyou et al.2013.Comparison in petroleum geology between Kuqa depression and southwest depression in Tarim Basin and its exploration significance.Acta Petrolei Sinica,34(2):201—218.
胡望水,陈毓遂,肖安成等.1997.塔西南坳陷构造演化与含油气系统.石油勘探与开发,24(1):14—17.Hu Wangshui,Chen Yusui,Xiao Ancheng et al.1997.Tectonic evolution and petroleum system in the southwest depression of Tarim Basin.Petroleum Exploration and Development,24(1):14—17.
贾承造.1997.中国塔里木盆地构造特征与油气.北京:石油工业出版社.1—420.Jia Chengzao.1997.Tectonics Characteristics of the Tarim Basin in China and Its Oil-Gas Resources.Beijing:Petroleum Industry Press.1—420.
金之钧,王清晨.2007.中国典型叠合盆地油气形成富集与分布预测.北京:科学出版社.1—265.Jin Zhijun and Wang Qingchen.2007.Formation,Accumulation and Distribution Prediction of Oil-Gas Resources in the Typical Superimposed Basins,China.Beijing:Science Press.1—265.
刘生国,薛天庆,刘学锋.2000.塔里木盆地石炭—第四纪构造演化与地层组合特征.西安科技学院学报,20(2):128—130.Liu Shengguo,Xue Tianqing and Liu Xuefeng.2000.The Carboniferous-Quaternary tectonic evolution and stratigraphic assemblages characteristics of Tarim Basin.Journal ofXi'an University of Science&Technology,20(2):128—130.
刘亚雷,胡秀芳,王道轩等.2012.塔里木盆地三叠纪岩相古地理特征.断块油气田,19(6):696—700.Liu Yalei,Hu Xiufang,Wang Daoxuan et al.2012.Characteristics of Triassic lithofacies palaeogeography in Tarim Basin.Fault-Block Oil&Gas Field,19(6):696—700.
潘长春,周中毅,范善发等.1996.塔里木盆地热历史.矿物岩石地球化学通报,15(3):150—152.Pan Changchun,Zhou Zhongyi,Fan Shanfa et al.1996.Thermal history of Tarim Basin.Bulletin of Mineralogy,Petrology and Geochemistry,15(3):150—152.
邱楠生,胡圣标,何丽娟.2004.沉积盆地热体制研究的理论与应用.北京:石油工业出版社.122—132.Qiu Nansheng,Hu Shengbiao and He Lijuan.2004.Theory and Application of Thermal Regime in Sedimentary Basins.Beijing:Petroleum Industry Press.122—132.
汤良杰.1994.塔里木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.
唐武,王英民,张雷等.2013.塔里木盆地三叠纪前缘隆起迁移演化规律.古地理学报,15(2):219—230.Tang Wu,Wang Yingmin,Zhang Lei et al.2013.Forebulge migration and evolution of the Triassic in Tarim Basin.Journal of Palaeogeography,15(2):219—230.
田作基.2006.塔北前陆盆她与南天山造山带的耦合关系及油气分布特征.石油地质,11(4):16—20.Tian Zuoji.2006.Coupling relation between Tabei foreland basin and Nantianshan orogenic belt and their oil-gas distribution feature.Petroleum Geology,11(4):16—20.
王飞宇,张水昌,张宝民等.2003.塔里木盆地寒武系海相烃源岩有机成熟度及演化史.地球化学,32(5):461—468.Wang Feiyu,Zhang Shuichang,Zhang Baomin et al.2003.Maturity and its history of Cambrian marine source rocks in the Tarim Basin.Geochimica,32(5):461—468.
萧德铭,冯子辉.1999.塔里木盆地大庆区块烃源岩演化史与油气成藏期研究.石油实验地质,21(1):28—33.Xiao Deming and Feng Zihui.1999.Study on the evolutionary history of source rock and the pool-forming periods of hydrocarbon in the Daqing block of the Tarim Basin.Experimental Petroleum Geology,21(1):28—33.
辛艳朋,邱楠生,李慧莉.2011.塔里木盆地下古生界烃源岩二次生烃范围研究.地球物理学报,s4(7):1863--1873.Xin Yanpeng,Qiu Nansheng and Li Huili.2011.The range of secondary hydrocarbon generation of Lower Palaeozoic source rock in Tarim Basin.Chinese Journal of Geophysics,54(7):1863^-1873.
邢卫新,汤达祯,马新海等.2007.塔里木盆地东北缘孔雀河地区烃源岩演化特征及成藏条件研究.天然气地球科学,18(1):57—61.Xing Wenxin,Tang Dazhen,Ma Xinhai et al.2007.Thermal evolution characteristics of hydrocarbon source rocks and pool forming conditions in the Kongque River area,northeastern fringe of Tarim Basin.Natural Gas Geoscience,18(1):57—61.
许杰.2009.塔里木盆地上泥盆统—石炭系层序地层学研究(博士学位论文).长沙:中南大学.1—222.Xu Jie.2009.Sequence Stratigrapy of Upper Devonian-Carboniferous in Tarim Basin(PhD Thesis).Changsha:Central South University.1—222.
许效松,刘宝珺,牟传龙等.2004.中国中西部海相盆地分析与油气资源.北京:地质出版社.47—55.Xu Xiaosong,Liu Baojun,Mou Chuanlong et al.2004.The Analysis of Marine Basins in Central and Western China and Its Hydrocarbon Resources.Beijing:Geological Publishing House.47-—55.
张斌,赵莆,张水昌等.2007.塔里木盆地和四川盆地海相烃源岩成烃演化模式探讨.科学通报,52(增刊):108—114.Zhang Bin,Zhao Zhe,Zhang Shuichang et al.2007.Discussion on marine source rooks thermal evoluement patterns in the Tarim Basin and Sichuan Basin,West China.Chinese Science Bulletin,52(suppl.):141—149.
张光亚,赵文智,王红军等.2007.塔里木盆地多旋回构造演化与复合含油气系统.石油与天然气地质,28(5):653—663.Zhang Guangya,Zhao Wenzhi,Wang Hongjun et al.2007.Multicycle tectonic evolution and composite petroleum systems in the Tarim Basin.Oil&Gas Geology,28(5):653—663.
张水昌,梁狄刚,张宝民等.2004a.塔里木盆地海相油气的生成.北京:石油工业出版社.1—200.Zhang Shuichang,Liang Digang,Zhang Baoming et al.2004.Marine Hydrocarbon Generation in the Tarim Basin.Beijing:Petroleum Industry Press.1—200.
张水昌,赵文智,王飞宇等.2004b.塔里木盆地东部地区古生界原油裂解气成藏历史分析——以荚南2气藏为例.天然气地球科学,15(5):441—451.Zhang Shuichang,Zhao Wenzhi,Wang Feiyu et al.2004.Paleozoic oil cracking gas accumulation history from eastern part of the Tarim Basin——A case study of the YN2 gas reservoir.Natural Gas Geoscience,15(5):441—451.
赵靖舟,李启明.2002.塔里术盆地克拉通区海相油气成藏期与成藏史.科学通报,47(增刊):116—121.Zhao Jingzhou and Li Qiming.2002.Timing and history of marine hydrocarbon accumulation in Tarim Craton.Chinese Science Bulletin,47(suppl.):120—127.
赵靖舟,李启明.2004.塔里木盆地油气藏形成与分布规律.北京:石油工业出版社.13—14.Zhao Jingzhou and Li Qiming.2004.Formation and Distribution of the Oil and Gas Reservoirs in the Tarim Basin.Beijing:Petroleum Industry Press.13—14.
朱如凯,罗平,罗忠.2002.塔里木盆地晚泥盆世及石炭纪岩相古地理.古地理学报,4(1):13—24.Zhu Rukai,Luo Ping and Luo Zhong.2002.Lithofacies palaeo-geography of the Late Devonian and Carboniferous in Tarim Basin.Journal of Palaeogeography,4(1):13—24.
Chen J S,Huang B C and Sun L S.2010.New constraints to the onset of the India-Asia collision:Paleomagnetic reconnaissance on the Linzizong Group in the Lhasa Block,China.Tectonophysics,489(1—4):189—209.
Kapp P,Yin A,Manning C E et al.2000.Blueschist-bearing metamorphic core complexes in the Qiangtang Block reveal deep crustal structure of northern Tibet.Geology,28(1):19—22.
Li M J,Wang T G,Chen J F et al.2010.Paleo-heat flow evolution of the Tabei uplift in Tarim Basin,Northwest China.Journal of Asian Earth Sciences,37(1):52—66.
Qiu N S,Chang J,Zuo Y H et al.2012.Thermal evolution and maturation of Lower Paleozoic source rocks in the Tarim Basin,Northwest China.AAPG Bulletin,96(5):789—821.
Robinson A C,Yin A,Manning C E et al.2004.Tectonic evolution of the northeastern Pamir:Constraints from the northern portion of the Cenozoic Kongur Shan extensional system,western China.GSA Bulletin,116(7—8):953—973.
Sobel E R.1999.Basin analysis of the Jurassic-Lower Cretaceous Southwest Tarim Basin,Northwest China.GSA Bulletin,111(5):709—724.
Vandenbroucke M,Behar F and Rudkiewicz J L.1999.Kinetic modelling of petroleum formation and cracking-Implications from the high pressure/high temperature Elgin Field(UK,North Sea).Organic Geochemistry,30(9):1105—1125.
Yin A and Harrison T M.2000.Geologic evolution of the Himalayan-Tibetan orogen.Annual Review of Earth and Planetary Sciences,28:211—280.
Zhang Q,Huang H,Zheng L et al.2007.Secondary hydrocarbon generation potential from heavy oil,oil sand and solid bitumen during the artificial maturation.Organic Geochemistry,38(12):2024—2035.
Zhu D C,Zhao Z D,Niu Y L et al.2013.The origin and pre-Cenozoic evolution of the Tibetan Plateau.Gondwana Research,23(4):1429—1454.
①金之钧等.2003.塔里木盆地台盆区有效烃源及油气勘探方向.中石化西指研究报告.
②谢觉新,周中毅,潘长春等.1994.塔里木盆地古地温、热演化史及油气评价.“八五”国家重点科技攻关项目“塔里木盆地油气资源”成果报告.
③解启来,周中毅,施继锡.1998.塔里木盆地生油岩成熟度确定及成烃演化史研究.“九五”国家重点攻关项目“塔里木盆地石油天然气勘探”成果报告.
④张水昌,王飞宇,张俊等.2000.塔里木盆地油源对比、烃源岩生烃史及油气藏形成史.“九五”国家重点攻关项目“塔里木盆地石油天然气勘探(二期)”成果报告.
⑤胡德庆,柳德全.2003.塔里木盆地构造演化史与构造控油特征研究.中石化西指立项报告.