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Article Navigation >  Acta Sedimentologica Sinica  > 1996  >  14(4): 24-30

Lu Shuangfang, Wang Ziwen, Fu Xiaotai, Wang Zhenping. Calibration of the Reactive Kinetic Model of Hydrocarbon Gene ration of Vitrinite and its Application in Restoring Paleo heat History of Huhehu Depression, Hailar Basin[J]. Acta Sedimentologica Sinica, 1996, 14(4): 24-30.
Citation: Lu Shuangfang, Wang Ziwen, Fu Xiaotai, Wang Zhenping. Calibration of the Reactive Kinetic Model of Hydrocarbon Gene ration of Vitrinite and its Application in Restoring Paleo heat History of Huhehu Depression, Hailar Basin[J]. Acta Sedimentologica Sinica, 1996, 14(4): 24-30.
shu

Calibration of the Reactive Kinetic Model of Hydrocarbon Gene ration of Vitrinite and its Application in Restoring Paleo heat History of Huhehu Depression, Hailar Basin

  • Daqing Petroleum Institute,Anda 151400

  • Received Date: 1995-01-01
  • Publish Date: 1996-12-10
  • The vitrinite reflectance (R o) is related to its hydrocarbon generation ratio, therefore, the hydrocarbon yielding could be calculated from its R o value. Meanwhile, having calibrated the reactive kinetic parameters of hydrocarbon generation of vitrinite, we can calculate its hydrocarbon yielding if its paleo heat history is known. On the contrary, if when the hydrocarbon yielding is known, it is possible to deduce the heating history it experienced.Based on this basic principle, the kinetic model of hydrocarbon generation of vitrinite is constructed and calibrated, and the theoretical model of restoring paleo heat history, which can be used in sophisticated geological conditions such as in a region once undergone uplift, erosion or non linear variation of paleo teperature, is set up.Combined with measured R o values of practical samples, the paleo heat history of Haican-7 Well is recovered effectively.
  • [1] (1) 卢双舫等. 煤岩显微组分的成烃动力学. 中国科学 (B辑 ), 1995, 25 (1): 101-107.

    (2) 李维铮等. 运筹学. 北京: 清华大学出版社, 1982.

    (3) 庞雄奇等. 含油气盆地史、 热史、 生留排烃史数值模拟研究与烃源岩定量评价. 北京: 地质出版社, 1993.

    (4) Lerche I. Determination of paleoheat flux from vitrinite reflectance. AAPG., 1984, 68 (11): 1704-1717.

    (5) Royden L, et al. Continental margin subsidence and heatflow: Important parameters in formation of petroleum hy-drocarbons. AAPG Bull., 1980, 64.
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Publishing history
  • Received:  1995-01-01
  • Published:  1996-12-10

Calibration of the Reactive Kinetic Model of Hydrocarbon Gene ration of Vitrinite and its Application in Restoring Paleo heat History of Huhehu Depression, Hailar Basin

  • Daqing Petroleum Institute,Anda 151400
  • Received Date: 1995-01-01
  • Publish Date: 1996-12-10

Abstract: The vitrinite reflectance (R o) is related to its hydrocarbon generation ratio, therefore, the hydrocarbon yielding could be calculated from its R o value. Meanwhile, having calibrated the reactive kinetic parameters of hydrocarbon generation of vitrinite, we can calculate its hydrocarbon yielding if its paleo heat history is known. On the contrary, if when the hydrocarbon yielding is known, it is possible to deduce the heating history it experienced.Based on this basic principle, the kinetic model of hydrocarbon generation of vitrinite is constructed and calibrated, and the theoretical model of restoring paleo heat history, which can be used in sophisticated geological conditions such as in a region once undergone uplift, erosion or non linear variation of paleo teperature, is set up.Combined with measured R o values of practical samples, the paleo heat history of Haican-7 Well is recovered effectively.

Lu Shuangfang, Wang Ziwen, Fu Xiaotai, Wang Zhenping. Calibration of the Reactive Kinetic Model of Hydrocarbon Gene ration of Vitrinite and its Application in Restoring Paleo heat History of Huhehu Depression, Hailar Basin[J]. Acta Sedimentologica Sinica, 1996, 14(4): 24-30.
Citation: Lu Shuangfang, Wang Ziwen, Fu Xiaotai, Wang Zhenping. Calibration of the Reactive Kinetic Model of Hydrocarbon Gene ration of Vitrinite and its Application in Restoring Paleo heat History of Huhehu Depression, Hailar Basin[J]. Acta Sedimentologica Sinica, 1996, 14(4): 24-30.
shu

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