Hydrocarbon accumulation in deep fluid modified carbonate rock in the Tarim Basin

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• 作者：XiuXiang Lü (1) (2)
  QiLai Xie (3)
  Ning Yang (1) (2)
  JianJiao Li (1) (2)
  
• 关键词：deep fluid ; carbonate rock ; hydrocarbon accumulation ; the Tarim Basin
• 刊名：Chinese Science Bulletin
• 出版年：2007
• 出版时间：November 2007
• 年：2007
• 卷：52
• 期：1-supp
• 页码：184-192
• 全文大小：3018KB
• 参考文献：1. Budd D, Saller A, Harris P. Unconformities and porosity in carbonate strata. AAPG Memoir, 1995, 63
  2. Saller A, Dickson J, Matsuda F. Evolution and distribution of porosity associated with subaerial exposure in Upper Paleozoic plate form lime stones, West Texas. AAPG Bull, 1999, 83(11): 1835-854
  3. Hopkins J. Characterization of reservoir lithologies within sub unconformity pools: Pekisko formation, medicine river field, Alberta, Canada. AAPG Bull, 1999, 83(11): 1855-870
  4. Xia R Y, Tang J S, Guan B Z, et al. Ordovician palaeo-karst landform in Ordos’s basin and gas enrichment characteristics. Oil Gas Geol (in Chinese), 1999, 20(2): 133-36
  5. Jia Z Y, Cai Z X, Xiao Y R. Paleo-weathering crust: An important reservoir (body) type of carbonate rocks. Earth Sci-J China Univ Geosci (in Chinese), 1995, 20(3): 283-89
  6. Zhu L F. A diagenetic Model of the Formation of carbonate gas reservoirs in China. Acta Sed Sin (in Chinese), 1995, 13(2): 140-49
  7. Qiu Z J, Gong Z S. Oil and Gas Exploration in China (Volume II: Western Oil and Gas Area) (in Chinese). Beijing: Petroleum Industry Press. 1999
  8. Zhou X X. First discussion on network like oil and gas pools. Petrol Explor Dev (in Chinese), 2000, 27(3): 5-
  9. Gu J Y. Karst and Oil & Gas Distribution in Lunnan Buried Hill, Tarim Basin (in Chinese). Beijing: Petroleum Industry Press. 2001
  10. Yan X B, Han Z H, Li Y H. Reservoir characteristics and formation mechanisms of the Ordovician carbonate pools in the Tahe oilfield. Geol Rev (in Chinese), 2002, 48(6): 619-26
  11. Zhou H T, Gao C Q. The types of carbonate reservoir in Tahe oilfield. Geophys Prosp Petrol (in Chinese), 2005, 44(1): 37-0
  12. Schrijver K, Williams-Jones A E, Bertrand R, et al. Genesis and controls of hydrothermal dolomitization in sandstones of the application thrust belt, Quebec, Canada: Implication for associated galena-barite mineralization. Chem Geol, 1996, 129: 257-79 CrossRef
  13. Tritlla J, Cardellach E, Sharp Z D. Origin of vein hydrothermal carbonates in Triassic limestones of the Espadan Ranges Iberian Chain, E Spain. Chem Geol, 2001, 172: 291-05 CrossRef
  14. Gillhausa A, Richter D K & Meijer J, et al. Quantitative high resolution cathodoluminescence spectroscopy of diagenetic and hydrothermal dolomites. Sediment Geol, 2001, 140: 191-99 CrossRef
  15. Duggan J P, Mountjoy E W & Stasiuk L D. Fault-controlled dolomitization at Swan Hills Simonette oil field (Devonian), deep basin west-central Alberta, Canada. Sedimentology, 2001, 48: 301-23 CrossRef
  16. Auajjar J, Boulegue J, Dolomites in the Tazekka Pb-Zn district, eastern Morocco: Polyphase origin from hydrothermal fluids. Terra Nova, 2002, 14: 175-82 CrossRef
  17. Guedes S C, Rosière C A, Barley M E, et al. The association of carbonate alteration of banded iron formation with the Carajás high-grade hematite deposits. Appl Earth Sci, 2003, 12: 26-5 CrossRef
  18. Al-Aasm I. Origin and characterization of hydrothermal dolomite in the Western Canada Sedimentary Basin. J Geochem Explor, 2003, 78-9: 9-5 CrossRef
  19. Green D, Mountjoy E W. Fault and conduit controlled burial dolomitization of the Devonian west-central Alberta Deep Basin. Bull Can Petrol Geo, 2005, 53(2): 101-29 CrossRef
  20. Zhao J Z, Pang W, Wu S B, et al. Geochronology and characteristics of marine hydrocarbon accumulation in the Tarim Basin. Chin J Geol (in Chinese), 2002, 37(Suppl): 81-0
  21. Wyllie P J. Magmatic consequences of volatile fluxes from the mantle. In: Perchuk L L, ed. Progress in Metamorphic and Magmatic Petrology. London: Cambridge University Press, 1991, 477-03
  22. Li M C, Li J, Wan Y J. Fluids in the sedimentary basin. Acta Petrolei Sin, 2001, 22(4): 13-8
  23. Preparatory Committee of Fluid Earth Science of the Chinese Geophysical Society. The current status of mantle fluids researches and their prospectives in China. Chin J Geophys, 40(Suppl): 1997, 60-9
  24. Fyfe W S. Deep fluids and volatile recycling: crust to mantle. Tectonophys, 1997, 275: 243-51 CrossRef
  25. Scambelluri M, Philippot P. Deep fluids in subduction zones. Lithos, 2001, 55: 213-27 CrossRef
  26. Zhang M J, Wang X B, Hu P Q, et al. The chemical compositions of volatiles in upper mantle and their implication for hydrocarbon generation. Nat Gas Geosci (in Chinese), 2006, 17(1): 31-4
  27. Frape S, Blyth A, Blomqvist R, et al. Deep fluids in the continents: II. Crystalline rocks. In: Drever J, ed. Treatise on Geochemistry 5 Surfaces and Ground Water, Weathering, and Soils. Amsterdam: Elsevier, 2004, 541-80
  28. Stober I, Bucher K. Deep-fluids: Neptune meets Pluto. Hydrogeo J, 2005, 13(1): 112-15 CrossRef
  29. Jin Z J, Yang L, Zeng J H, et al. Deep fluid activities and their effects on generation of hydrocarbon in Dongying depression. Petrol Explor Dev (in Chinese), 2002a, 29(2): 42-4
  30. Jin Z J, Zhang L P, Zeng J H, et al. Primary study of geochemical features of deep fluids and their effectiveness on oil/gas reservoir formation in sedimental basins. Earth Sci J China Univ Geosci (in Chinese), 2002b, 27(6): 659-64
  31. Wang X B, Liu G, Chen J F, et al. Fluid in the earth. Earth Sci Front (in Chinese), 1996, 3(3): 105-18
  32. Wen S M, Wang J Z, Wang G Z. Igneous rock features and the impact to the hydrocarbon accumulation in Tarim Basin. Oil Geophys Prosp (in Chinese), 2005, 40(Supp 1): 33-9
  33. Xu Y C, Sheng P, Tao M X, et al. Distribution of the nature gas He isotope in the Petroliferous Basin, China. Chin Sci Bull (in Chinese). 1994, 39(16): 1505-508
  34. Zheng J J, Sun G Q, Sun S L, et al. Contrasting the helium isotopic com position of natural gas in Tarim Basin with that in east China oil and gas basins. Nat Gas Ind (in Chinese), 2004, 24(9): 26-9
  35. Zhang X B, Xu Y C, Sun M L, et al. Discovery and its geological significance of the mantle helium in the reservoir fluid inclusions from Huanghua depression. Sci China Ser D-Earth Sci (in Chinese), 2003, 33(7): 673-78
  36. Zhang J L. Formation mechanism of the Silurian solid asphalt sandstone in the Tarim Basin. In: Zhang Y W, ed. Papers of the International Symposium on Formation Mechanism of Oil-Gas Reservoirs and Hydrocarbon Resources Evaluation (in Chinese). Beijing: Petroleum Industry Press, 1997: 247-52
  37. Zhang J L, Zhu B Q, Zhang P Z, et al. Pb Sr Nd isotopic systematics of kerogen and bitumen in the Tarim Basin and their implications for its origin and evolution Sci Geol Sin (in Chinese), 1998, 33(3): 310-17
  38. Chen J G, Li X W, Yu B G, et al. Geochemical characteristics and its lithosphere evolution significance of the black shales which come from the bottom of the lower Cambrian, Tarim Basin. Sci China Ser D-Earth Sci (in Chinese), 2002, 32(5): 374-82
  39. Huang D Z, Gao J, Dai T G, et al. The source of the deep fluid in the west Tianshan ancient subduction zone-The isotope evidence of the Pb and Sr from the main rock and high pressure connections in the high-pressure metamorphic belt. Sci China Ser D-Earth Sci (in Chinese), 2004, 34(9): 835-44
  40. Zhou S X, Ye X R. Rare gas isotopic composition of the deep carbonate rocks, Tarim Basin. Chin Sci Bull (in Chinese), 2002, 47(4): 313-17
  41. Wang G A, Shen J Z, Ji M Y. Carbon isotopic composition and origin of carbon dioxide in natural gases in northern and central Tarim Basin. Geol-Geochem (in Chinese), 2001, 29(1): 36-9
  42. Zhou S X, Wang X B, Meng Z F, et al. Composition of the gas inclusion and its C isotope of the deep carbonate rocks in the Tarim Basin. Sci China Ser D-Earth Sci (in Chinese), 2003, 33(7): 665-72
  43. Jiang M S, Zhu J Q, Chen D Z, et al. Characteristics of the C and Sr isotope from the Ordovician carbonate and the response to the sea level change. Sci China Ser D-Earth Sci, 2003, 33(7): 665-72
  44. Huang S J, Liu S G, Li G R, et al. Strontium isotope composition of marine carbonate and the influence of diagenetic fluid on it in Ordovician. J Chengdu Univ Tech (Sci Tech Ed)(in Chinese), 2004, 31(1): 1-
  45. Liu Z L, Xia B. The genesis of molecular nitrogen of natural gases and its exploration risk coefficient in Tarim Basin. Nat Gas Geosci (in Chinese), 2005, 16(2): 224-28
  46. Zheng D Z, Zheng R F. A approach to the ore-forming mechanism for fluorite deposits. Acta Geol Sichuan (in Chinese), 2005, 25(3): 149-55
  47. Zhu D Y, Hu W X, Song Y C, et al. Fluoritization in Tazhong 45 reservoir: Characteristics and its effect on the reservoir bed. Acta Petrol Et Mineralogica (in Chinese), 2005, 24(3): 205-15
  48. Jin Z J, Zhu D Y, Hu W X, et al. Geological and geochemical signatures of hydrothermal activity and their influence on carbonate reservoir beds in the Tarim Basin. Acta Geol Sin (in Chinese), 2006, 80(2): 245-53
  49. Condie K C. Another look at rare earth elements in shaces. Geochim et Cosmochim Acta, 1991, 55: 2527-531 CrossRef
  50. Mclennan S M. Rare earth elements in sedimentary rocks: Influence of proverance and sedimentary processes. In: Lipin B R, Mckay G A, eds. Geochemistry and Mineralogy of Rare Earth Elements, Miner Soc A Rev Miner, 1989, 21: 169-00
  51. Zhou T F, Yue S C, Lan T Y. Sulfur isotope geochemistry of the Anqing copper deposit. Earth Sci (in Chinese), 1995, 20(6): 705-11
  52. Chen X P, Gao J Y, Cao J C. Barite and fluorite deposit in China. In: The Committer of the “Deposits in China- ed. Deposit in China (Series II) (in Chinese). Beijing: Geology Press, 1994. 281-40
  53. Claypool G E, Holster W T, Kaplan I R, et al. The age curves of sulphur and oxygen isotopes in marine sulphate and their mutual interpretation. Chem Geol, 1980, 28: 199-60 CrossRef
  54. Holser W T, Magaritz M, Ripperdan R L. Global isotopic events. In: Walliser O H, ed. Global Events and Event Stratigraphy in the Phanerzoic. Berlin: Springer-Verlag, 1996. 63-8
  55. Tao H X, Xu Y X. Hydrothermal fluid and hydrocarbon reservoir. Petrol Explor Devel (in Chinese), 1994, 21(6): 92-7
  56. Gao B, Tao M X, Wang W C, et al. Influences of deeply sourced thermal fluid on the formation of hydrocarbon reservoirs. Bull Miner Petrol Geochem (in Chinese), 2001, 20(1): 30-4
  57. Gao Y Q, Liu L. Brief introduction of effect of magma intrusion activity on sandstone. Geo Sci Tech Information (in Chinese), 2003, 22(2): 13-6
  58. Falignati P, Malfitano G, Sbrana A. The / Pantelleria calgera geothermal system: Data from the hydrothermal minerals. J Volcanol Geotherm Res, 1997, 75: 251-70 CrossRef
  59. Kappler P, Zeeh S. Relationship between fluid flow and faulting in the Alpine realm (Austria, Germany, Italy). Sediment Geol, 2000, 131: 147-62 CrossRef
  60. Marty B, Dauphas N. The nitrogen record of crust-mantle interaction and mantle convection from Archean to Present. Earth Planet Sci Lett, 2003, 206: 397-10 CrossRef
  61. Zhang M J, Wang X B, Li L W. Composition of mantle fluid. Earth Sci Front (in Chinese), 2000, 7(2): 401-12
  62. Teng Y G, Liu J D, Zhang C J, et al. Geological and geochemical information of deep ore fluid in Lanping basin, Yunnan Province. Contrib Geo Miner Resour Res (in Chinese), 2000, 15(4): 314-19
  63. Teng J W. Dynamic process of substance and energy exchanges in depths of the earth and formation of mineral resources. Geotectonica et Metallogenia (in Chinese), 2003, 27(1): 3-1
  64. Mao J W, Li X F. Mantle-derived fluids in relation to ore-forming and oil-forming processes. Mineral Deposits (in Chinese), 2004, 23(4): 520-32
  65. Aquilina L, Ladouche B, Doerfliger N. Origin, evolution and residence time of saline thermal fluids (Balaruc springs, southern France): Implications for fluid transfer across the continental shelf. Chem Geol, 2002, 192: 1-1 CrossRef
  66. Hecht L, Freiberger R, Gilg H A, et al. Rare earth element and isotope (C, O, and Sr) characteristics of hydrothermal carbonates: Genetic implications for dolomite-hosted talc mineralization at Gopfersgrun Fichtelgebirge, Germany. Chem Geol, 1999, 155: 115-30 CrossRef
  67. Bell D R, Grégoire M, Grove T L, et al. Silica and volatile-element metasomatism of Archean mantle: A xenolith-scale example from the Kaapvaal Craton. Contrib Mineral Petrol, 2005, 150: 251-67 CrossRef
  68. Yang N, Lu X X, Zheng D M. Alteration of the igneous rock on the carbonate reservoirs in Tarim Basin. J Xi’an Shiyou Univ (Nat Sci Ed)(in Chinese), 2005, 20(4): 1-
  69. Liu Y K, Zheng D M, Wang J N, et al. The Ordovician carbonate reservoir characteristics and mineralization in Yingmaili low heave of Tarim Basin. Nat Gas Geo (in Chinese), 2005, 16(5): 587-91
  70. Xia Riyuan, Tang Jiansheng & Luo Wweiquan, et al. New progress of oil and gas fields-paleo-karst and deep karst. Carsologica Sin (in Chinese), 2001, 20(1): 76
  71. Wang S M, Jin Z J, Xie C L. Transforming effect of deep fluids on carbonate reservoirs in the Well TZ45 region. Geo Rev (in Chinese), 2004, 50(5): 543-47
  72. Lv X X, Yang N, Xie Q L, et al. Carbonate reservoirs transformed by deep fluid in Tazhong area. Oil Gas Geo (in Chinese), 2005, 26(3): 284-89
  73. Zhang R H, Hu S M. Dissolved kinetics and surface chemistry of the fluorite in the flows system. Sci China Ser D-Earth Sci (in Chinese), 1996, 26(1): 41-1
  74. Zhang R, Hu S M. Experimental observation of deep crust fluid NaCl aqueous solution at elevated temperatures and pressures and its significance. Chin Sci Bull, 1999, 44(7): 654-60 CrossRef
  75. Zhou X Y, Wang Z M, Yang H J, et al. Cases of discovery and exploration of marine fields in China (part 5): Tazhong Ordovician condensate field in Tarim Basin. Marine Origin Petrol Geol (in Chinese), 2006, 11(1): 45-1
  76. Jia C Z. Plate Tectonics and Continental Dynamics of Tarim Basin (in Chinese). Beijing: Petroleum Industry Press, 2004, 127-28
  
• 作者单位：XiuXiang Lü (1) (2)
  QiLai Xie (3)
  Ning Yang (1) (2)
  JianJiao Li (1) (2)
  
  1. Basin & Reservoir Research Center, China University of Petroleum, Beijing, 102249, China
  2. State Key Laboratory of Petroleum Resource and Prospecting, China University of Petroleum, Beijing, 102249, China
  3. School of Resource and Environment, Agriculture University of South China, Guangzhou, 510642, China
  
• ISSN：1861-9541

文摘

The activities of deep fluid are regionalized in the Tarim Basin. By analyzing the REE in core samples and crude oil, carbon isotope of carbon dioxide and inclusion temperature measurement in the west of the Tazhong Uplift in the western Tarim Basin, all the evidence confirms the existence of deep fluid. The deep fluid below the basin floor moved up into the basin through discordogenic fault and volcanicity to cause corrosion and metasomatosis of carbonate rock by exchange of matter and energy. The pore structure and permeability of the carbonate reservoirs were improved, making the carbonate reservoirs an excellent type of deeply buried modification. The fluorite ore belts discovered along the large fault and the volcanic area in the west of the Tazhong Uplift are the outcome of deep fluid action. Such carbonate reservoirs are the main type of reservoirs in the Tazhong 45 oilfield. The carbonate reservoirs in well YM 7 are improved obviously by thermal fluid dolomitization. The origin and territory of deep fluid are associated with the discordogenic fault and volcanicity in the basin. The discordogenic fault and volcanic area may be the pointer of looking for the deep fluid modified reservoirs. The primary characteristics of hydrocarbon accumulation in deep fluid reconstructed carbonate rock are summarized as accumulation near the large fault and volcano passage, late-period hydrocarbon accumulation after volcanic activity, and subtle trap reservoirs controlled by lithology.