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DUAN Yi, ZHANG Hui, ZHENG Chao-yang, WU Bao-xiang. Study on Genesis of Crude Oil from Qaidam Basin[J]. Acta Sedimentologica Sinica, 2004, 22(S1): 61-65.
Citation: DUAN Yi, ZHANG Hui, ZHENG Chao-yang, WU Bao-xiang. Study on Genesis of Crude Oil from Qaidam Basin[J]. Acta Sedimentologica Sinica, 2004, 22(S1): 61-65.

Study on Genesis of Crude Oil from Qaidam Basin

  • Received Date: 2003-12-29
  • Publish Date: 2004-12-10
  • Qaidam basin is one of the largest petroliferous basins in the northwestern China. After 50 years oil-gas exploration, 18 oil fields have been found in this basin, which are mainly distributed in the western portion of Qaidam basin. Their geneses are always the focus in which people are interested. The physical and chemical character, oil-rock correlation and genetic mechanism are studied, it is indicated that the western Qaidam and the northern Qaidam are two different oil-generating units, that they have obviously different oil-forming environments, precursor types, maturity and source of oil. Although organic carbon abundance of source rocks is low, plant lipids are well preserved in the reducing and saline acustrine environments. Plant lipids together with soluble organic matter and kerogen can generate a significant volume of crude oil at low mature stage and be the main way to produce immature and low mature crude oils in the western Qaidam basin
  • [1] 黄杏珍,邵宏舜,顾树松.柴达木盆地的油气形成与寻找油气田方向.兰州:甘肃科学技术出版社,1993. 363~370
    [2] 段毅,王智平,张晓宝,等.柴达木盆地西部原油极性化合物特征及其地球化学意义.地质学报,2003,77(3):414~422
    [3] Ritts B D, Hanson A D, Zinniker D, et al. Lower-Middle Jurassic no nmarine source rocks and petroleum systems of the northern Qaidam basin, northwe st China. AAPG Bulletin, 1999, 83: 1980~3200
    [4] Hanson A D, Ritts B D, Zinniker D, et al. Upper Oligocene lacustrine source rocks and petroleum systems of the northern Qaidam basin, northwest China. AAPG Bulletin, 2001, 85: 601~3619
    [5] 王铁冠,钟宁宁,侯读杰,等.低熟油气形成机理与分布.北京:石油工业出版社,1995
    [6] ten Haven H L, Leeuw J W de, Rullktter, et al. Restricted ut ility of the pristane/phytane ratio as a palaeoenvironmental indicator. Nature, 1987, 330: 641~3642
    [7] 包建平,王铁冠,干一女.脱羟基维生素E及其地球化学意义.江汉石油学院学报 ,1989,11(3):10~316
    [8] 段毅,彭德华,张晓宝,等. 柴达木盆地原油碳同位素组成的主控因素与成因类型. 沉积学报,2003,21(2):355~3359
    [9] Moldowan J M, Seifert W K, Gallegos E J. Relationship between petroleum composition and depositional environment of petroleum source rocks. AAPG B ulletin, 1985, 69: 1255~31268
    [10] Fu J G, Sheng P, Peng S C, et al. Peculiarities of salt lake sediments a s potential source rocks in China. Org Geochem, 1986, 10: 119~3126
    [11] Philp R P, Fan P, Lewis C A, et al. Geochemical characteristics of oils from Chaidamu, shanganning and Jianghan basins, China. Journal of Southeast Asian Earth Sciences, 1991, 5: 351~3358
    [12] Huang D F, Li J C, Zhang D J, et al. Maturation sequence of Tertiary crude oils in the Qaidam Basin and its significance in petroleum resource assessment. Journal of Southeast Asian Earth Sciences, 1991, 5: 359~3366
    [13] Mango F D. An invariance in the isoheptanes of petroleum. Science, 1987, 273: 514~3517
    [14] Mango F D. The origin of light hydrocarbons in petroleum: A kinetic test of the steady-state catalytic hypothesis. Geochimica et Cosmochimica Acta, 199 0, 54: 1315~31323
    [15] BeMent W O, Levey R A, Mango F D. The origin of oil generation as defined wi th a C7 chemistry parameter (2,4-DMP/2,3-DMP). Grimalt J O, Dorronsoro C . Organic Geochemistry: Developments and Application to Energy, Climate, Environ ment and Human History. A.I.G.O.A., San Sebastian, 1995. 505~3507
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  • Received:  2003-12-29
  • Published:  2004-12-10

Study on Genesis of Crude Oil from Qaidam Basin

Abstract: Qaidam basin is one of the largest petroliferous basins in the northwestern China. After 50 years oil-gas exploration, 18 oil fields have been found in this basin, which are mainly distributed in the western portion of Qaidam basin. Their geneses are always the focus in which people are interested. The physical and chemical character, oil-rock correlation and genetic mechanism are studied, it is indicated that the western Qaidam and the northern Qaidam are two different oil-generating units, that they have obviously different oil-forming environments, precursor types, maturity and source of oil. Although organic carbon abundance of source rocks is low, plant lipids are well preserved in the reducing and saline acustrine environments. Plant lipids together with soluble organic matter and kerogen can generate a significant volume of crude oil at low mature stage and be the main way to produce immature and low mature crude oils in the western Qaidam basin

DUAN Yi, ZHANG Hui, ZHENG Chao-yang, WU Bao-xiang. Study on Genesis of Crude Oil from Qaidam Basin[J]. Acta Sedimentologica Sinica, 2004, 22(S1): 61-65.
Citation: DUAN Yi, ZHANG Hui, ZHENG Chao-yang, WU Bao-xiang. Study on Genesis of Crude Oil from Qaidam Basin[J]. Acta Sedimentologica Sinica, 2004, 22(S1): 61-65.
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