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Article Navigation >  Acta Sedimentologica Sinica  > 2002  >  20(2): 320-325

WANG JianBao, GUO RuTai, XIAO XianMing, LIU ZuFa, SHEN JiaGui. Timing and Phases of Hydrocarbon Migration and Accumulation of the Formation of Oil and Gas Pools in Lunnan Low Uplift of Tarim Basin[J]. Acta Sedimentologica Sinica, 2002, 20(2): 320-325.
Citation: WANG JianBao, GUO RuTai, XIAO XianMing, LIU ZuFa, SHEN JiaGui. Timing and Phases of Hydrocarbon Migration and Accumulation of the Formation of Oil and Gas Pools in Lunnan Low Uplift of Tarim Basin[J]. Acta Sedimentologica Sinica, 2002, 20(2): 320-325.
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Timing and Phases of Hydrocarbon Migration and Accumulation of the Formation of Oil and Gas Pools in Lunnan Low Uplift of Tarim Basin

  • State Key Laboratory of Organic Geochemistry,Guangzhou Institute of Geochemistry,Chinese Academy of Sciences,Guangzhou 510640

  • Received Date: 2001-03-13
  • Rev Recd Date: 2001-08-30
  • Publish Date: 2002-04-10
  • Lower Palaeozoic strata in the Lunnan Low Uplift,of Tarim Basin, China, have recently been found to contain abundant migrated solid bitumen and petroleum-bearing fluid inclusions. In order to determine their origin and timing of the formation, bitumen/inclusion-rich core samples recovered from several wells in the area (mainly carbonate reservoir rocks and carrier units) were examined using a combination of organic petrographic and microthermometric techniques. Based on bitumen reflectance (BR o) measurements, solid bitumens were divided into three main groups, viz. (I) 1.20%～1.35%, (II) 0.80%～0.95% and (III) 0.05% . Hydrocarbon fluid inclusions were also grouped into three different assemblages based on their fluorescence colour and homogeneous temperatures ( T h): (I) yellow-green, T h = 80～90℃; (II) green, T h = 60～70℃ and (III) blue-green fluorescence, T h = 100～150℃. Spatial distributions of fluid inclusion Groups I, II and III within the structure closely match ed those for bitumen Groups I, II and III, respectively, and indicated that there were three separate episodes of large-scale oil migration and accumulation in the uplift. Using the BR o and inclusion Th data in combination with available burial and geothermal history in formation for the area, it was concluded that three corresponding phases of petroleum generation and migration took place during (I) Silurian to early Devonian, (II) Cretaceous to early Tertiary and (III) late Tertiary, from Cambrian-Ordovician source rocks. These findings provide useful insights into the complex origins of oil and gas pools in this region of Tarim Basin.
  • [1] 1. 冯祺，周东征，康利平等。塔北隆起新和-轮台断裂带构造特征及其控油性[A].童晓光，梁狄刚主编。塔里木盆地油气勘探论文集[C].乌鲁木齐:新疆科技卫生出版社，1991.267～273 [Feng Q,Zhou D Z,and Wang G.Tectonic features and its control on oil and gas pools of Taibei Uplift[A].In:Tong X G,Liang D G,eds.Paper Compilation of Oil and Gas Formation in the Tarim Basin[C].Urumqi:Xinjiang Science and Sanitation Press,1991.267～273]

    2. 刘登明。轮南地区构造演化的特点及其对油气藏形成的影响[A].童晓光，梁狄刚主编。塔里木盆地油气勘探论文集[C].乌鲁木齐:新疆科技卫生出版社，1991.274～279 [Liu D M.Tectonic evolution and its effect on the formation of oil and gas pools in the Lunnan Area[A].In:Tong X G,Liang D G,eds.Paper Compilation of Oil and Gas Formation in the Tarim Basin[C].Urumqi:Xinjiang Science and Sanitation Press,1991.247～279]

    3. 贾承造，李小池等。塔里木盆地油气藏形成条件及油气富集规律[A].北京石油勘探开发科学研究院。"八五"国家重点科技攻关项目成果报告（85-101-01-02）[R].1995.1～2,85～101 [Jia C Z,Li X Z,et al.Formation conditions and petroleum accumulation pattern of the Tarim Basin [A].Beijing Institute of Petroleum Development and Exploration ,Internal report of state key project,1995.1～2,85～101]

    4. 刘昌玉，陈永武。轮南断垒带三迭系石油地质特征和油气聚集规律的研究[A].童晓光，梁狄刚主编。塔里木盆地油气勘探论文集[C].乌鲁木齐:新疆科技卫生出版社，1991.497～504 [Liu C Y,Chen H W.The petroleum geological characteristics and distribution pattern of oil and gas pools of Triassic strata in the Lunnan Area,Tarim Basin[A].In:Tong X G,Liang D G,eds.Paper Compilation of Oil and Gas Formation in the Tarim Basin[C].Urumqi:Xinjiang Science and Sanitation Press,1991.497～504]

    5. 覃汉生，郭建华，赵妮。塔里木盆地轮南地区奥陶系油气藏圈闭成因分析及油气藏类型[A].童晓光，梁狄刚主编。塔里木盆地油气勘探论文集[C].乌鲁木齐:新疆科技卫生出版社，1991.545～551 [Tan H S,Guo G H,Zhou L.Origin of trapping structures and types of oil and gas pools in Ordovician strata in the Lunnan Area of the Tarim Basin[C] .In:Tang X G,Liang D G,eds.Paper Compilation of Oil and Gas Formation in the Tarim Basin[C].Urumqi:Xinjiang Science and Sanitation Press,1991.545～551]

    6. 周光熙，黄宏伟，石强。塔北隆起油气藏类型及其地质特征[A].童晓光，梁狄刚主编。塔里木盆地油气勘探论文集[C].乌鲁木齐:新疆科技卫生出版，1991.574～588 [Zhou G X,Huang H W,Shi C.Types of oil and gas pools and their geological characteristics in the Taibei Uplift,Tarim Basin[A].In:Tang X G,Liang D G,eds.Parper Compilation of Oil and Gas Formation in the Tarim Basin[C].Urumqi:Xinjiang Science and Sanitation Press,1991.574～588 ]

    7. 黄传波。塔里木盆地寒武-奥陶系碳酸盐岩油气藏形成条件[J].新疆石油地质，2000,21（3）:188～192 [Huang C B.Formation and distribution of oil and gas pools in the Taibei Uplift of the Tarim Basin[J].Xinjiang Petroleum Geology,1998,19（5）:357～361 ]

    8. 黄传波。塔里木盆地塔北隆起油气藏形成及分布规律[J].新疆石油地质，1998,19（5）:357～361 [Huang C B.Geological conditions to form oil and gas pools in Cambrian-Ordovician strata in the Tarim Basin[J].Xinjiang Petroleum Geology,2000,21（3）:188～192 ]

    9. 顾乔元，潘文庆，曹淑珍。轮南地区奥陶系油气藏特征[J].新疆石油地质，1999,20（3）:210～212[Gu Q Y,Pan W Q,Chao S Z.Characteristics of oil and gas pools in Ordovician strata in the Lunnan Area[J].Xinjiang Petroleum Geology,1999,20（3）:210～212 ]

    10. 肖贤明。塔里木盆地三叠系烃源岩有机岩石学特征与生烃评价[J].地球化学，1997,26（1）:64～71 [Xiao X M.Organic petrological characteristics of Triassic source rocks and its petroleum potentials in the Tarim Basin[J].Geochemistry,1997,26（1）:64～71 ]

    11. 梁狄刚，张水昌，王飞宇等。塔里木盆地生油岩与油源研究[A].北京石油勘探开发科学研究院。1996-111-01-03报告[R].1998 [Liang D G.Zhang,S C,Wang F Y.Study on source rocks and oil sources in the Tarim Baisn[A].Internal Report （1996-111-01-03）[R].Beijing Institute of Petroleum Exploration and Development,1998 ]

    12. 黄第藩，梁狄刚。塔里木盆地油气生成与演化[A].北京石油勘探开发科学研究院。"八五"国家重点科技攻关项目成果报告（85-101-01-04）[C].1995 [Huang D F,Liang D G.Formation and evolution of the Tarim Basin.Internal report （85-101-01-04）[R].Beijing Institute of Petroleum Exploration and Development,1995 ]

    13. Xiao Xianming,Liu Zufa,Liu Dehan,et al.A new method to reconstruct hydrocarbon-generating histories of source rocks in a petroleum-bearing basin--the method of geological and geochemical sections[J].Chinese Science Bulletin,2000,45（Supplemene）: 97～104

    14. 肖贤明，刘德汉，傅家谟。应用沥青反射率推算油气生成与运移的地质时间[J].科学通报，2000,45（19）:2 123～2 127 [Xiao X M,Liu D H,Fu J M.Dating hydrocarbon generation and migration by means of bitumen reflectance[J].Chinese Science Bulletin,2001,46（7）:610～614]

    15. 金奎励主编。有机岩石学研究--以塔里木盆地为例[M].北京:地震出版社，1997.155～180 [Jin K L.Organic Petrology-a Caes Study of the Tarim Basin[M].Beijing:Seismic Press,1997.155～180]
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  • Received:  2001-03-13
  • Revised:  2001-08-30
  • Published:  2002-04-10

Timing and Phases of Hydrocarbon Migration and Accumulation of the Formation of Oil and Gas Pools in Lunnan Low Uplift of Tarim Basin

  • State Key Laboratory of Organic Geochemistry,Guangzhou Institute of Geochemistry,Chinese Academy of Sciences,Guangzhou 510640
  • Received Date: 2001-03-13
  • Rev Recd Date: 2001-08-30
  • Publish Date: 2002-04-10

Abstract: Lower Palaeozoic strata in the Lunnan Low Uplift,of Tarim Basin, China, have recently been found to contain abundant migrated solid bitumen and petroleum-bearing fluid inclusions. In order to determine their origin and timing of the formation, bitumen/inclusion-rich core samples recovered from several wells in the area (mainly carbonate reservoir rocks and carrier units) were examined using a combination of organic petrographic and microthermometric techniques. Based on bitumen reflectance (BR o) measurements, solid bitumens were divided into three main groups, viz. (I) 1.20%～1.35%, (II) 0.80%～0.95% and (III) 0.05% . Hydrocarbon fluid inclusions were also grouped into three different assemblages based on their fluorescence colour and homogeneous temperatures ( T h): (I) yellow-green, T h = 80～90℃; (II) green, T h = 60～70℃ and (III) blue-green fluorescence, T h = 100～150℃. Spatial distributions of fluid inclusion Groups I, II and III within the structure closely match ed those for bitumen Groups I, II and III, respectively, and indicated that there were three separate episodes of large-scale oil migration and accumulation in the uplift. Using the BR o and inclusion Th data in combination with available burial and geothermal history in formation for the area, it was concluded that three corresponding phases of petroleum generation and migration took place during (I) Silurian to early Devonian, (II) Cretaceous to early Tertiary and (III) late Tertiary, from Cambrian-Ordovician source rocks. These findings provide useful insights into the complex origins of oil and gas pools in this region of Tarim Basin.

WANG JianBao, GUO RuTai, XIAO XianMing, LIU ZuFa, SHEN JiaGui. Timing and Phases of Hydrocarbon Migration and Accumulation of the Formation of Oil and Gas Pools in Lunnan Low Uplift of Tarim Basin[J]. Acta Sedimentologica Sinica, 2002, 20(2): 320-325.
Citation: WANG JianBao, GUO RuTai, XIAO XianMing, LIU ZuFa, SHEN JiaGui. Timing and Phases of Hydrocarbon Migration and Accumulation of the Formation of Oil and Gas Pools in Lunnan Low Uplift of Tarim Basin[J]. Acta Sedimentologica Sinica, 2002, 20(2): 320-325.
shu

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