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Tuo Jincai, Zeng Fangang, Huang Xinzheng, Ma Wanyi. Biyang Depression- An Example of Lacustrine Carbonate as Source Rocks of Petroleum[J]. Acta Sedimentologica Sinica, 1997, 15(S1): 64-69.
Citation: Tuo Jincai, Zeng Fangang, Huang Xinzheng, Ma Wanyi. Biyang Depression- An Example of Lacustrine Carbonate as Source Rocks of Petroleum[J]. Acta Sedimentologica Sinica, 1997, 15(S1): 64-69.

Biyang Depression- An Example of Lacustrine Carbonate as Source Rocks of Petroleum

  • Received Date: 1996-12-30
  • The general characteristics of lacustrine carbonate source rocks are discussed in this paper, where the lacustrine carbonate ofHetaoyuan Formation, Tertiary, Biyang Depression, was taken as an example. That the composition characteristics, the contentsof organic matters, the transformative rate of hydrocarbons and the type of organic matters show that lacustrine carbonate sourcerocks are rich in oil-generating material, and the convincible oil-source rock correlation material indicates that lacustrine carbonatesnot only can generate oils, but also be the source rocks of commercial oils.
  • [1] Palaces J . G.,Carbonate tucks as source of petroleum: Geologicaland chemical characteristics and oil-source correlation, London,11th Wozld Petroleum Congress Proceedings, 1984, 2:31-43.
    [2] Palaces J. G. . Andets D. E. and King J. D.,卞良樵译.南佛罗里达盆地一碳酸盐生油岩的一个典型实例.碳酸盐岩石油地球化学及生油潜力.北京:科学出版社.1990. 85-119
    [3] Tissot B. and Welte D. H.,Peuoleum formation and occurrence:Berlin Springer-Verlag, 1978, 96
    [4] Rubenstein I.,Sieskind O. and Albrecht P.,Rearranged ster-anes in shale: occurrence and simulated fromation. Jour. Chem.Soc. Perkin Trans. I. 1975, 1833-1836.
    [5] Sieskind O.,Joly G. and Albrecht P.,Simulation of geochemicaluansformations of sterols: superacid effect of clay minerals.Geochimica et Cosmochimica Acta. 1979. 43:1675-1679.
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  • Received:  1996-12-30

Biyang Depression- An Example of Lacustrine Carbonate as Source Rocks of Petroleum

Abstract: The general characteristics of lacustrine carbonate source rocks are discussed in this paper, where the lacustrine carbonate ofHetaoyuan Formation, Tertiary, Biyang Depression, was taken as an example. That the composition characteristics, the contentsof organic matters, the transformative rate of hydrocarbons and the type of organic matters show that lacustrine carbonate sourcerocks are rich in oil-generating material, and the convincible oil-source rock correlation material indicates that lacustrine carbonatesnot only can generate oils, but also be the source rocks of commercial oils.

Tuo Jincai, Zeng Fangang, Huang Xinzheng, Ma Wanyi. Biyang Depression- An Example of Lacustrine Carbonate as Source Rocks of Petroleum[J]. Acta Sedimentologica Sinica, 1997, 15(S1): 64-69.
Citation: Tuo Jincai, Zeng Fangang, Huang Xinzheng, Ma Wanyi. Biyang Depression- An Example of Lacustrine Carbonate as Source Rocks of Petroleum[J]. Acta Sedimentologica Sinica, 1997, 15(S1): 64-69.
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