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Article Navigation >  Acta Sedimentologica Sinica  > 1995  >  13(S1): 147-150

Liu Luofu, Wang Weihua, Li Shuyuan. Investigation on Secondary Generation of Hydrocarbons by Thermal Modelling of Kerogen[J]. Acta Sedimentologica Sinica, 1995, 13(S1): 147-150.
Citation: Liu Luofu, Wang Weihua, Li Shuyuan. Investigation on Secondary Generation of Hydrocarbons by Thermal Modelling of Kerogen[J]. Acta Sedimentologica Sinica, 1995, 13(S1): 147-150.
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Investigation on Secondary Generation of Hydrocarbons by Thermal Modelling of Kerogen

  • University of Petroleum, Beijing 102200

  • Received Date: 1995-08-10
  • Publish Date: 1995-12-10
  • Based on results from thermal modelling experiments of kerogens,this paper presents a brief discussion on secondary generation of hydrocarbons. Geological effects, such as structural movement, etc.,may result in liftion or denudation of source rocks which do not enter highly-and post-mature phases, which causes the decrease of geotemperature of the source rocks and the cease of hydrocarbon generation. While the source rocks subside .again, the geotemperature increases, and when it reachs a certain point, the unexhaused kerogens may generate hydrocarbons again.The generated oil-gas amount with the continuous process of hydrocarbon generation is close to the total amounts of twice generations, indicating that hydrocarbon-generating amount is not affected by the secondary hydrocarbon generation that only defer generating oil and gas.
  • [1] 1.梁狄刚、王会样，1992，塔里木盆地油源问题，见:塔里木盆地油气勘探论文集，童晓光、梁狄刚主编，乌鲁木齐:新疆科技卫生出版社(K) , 321-330。

    2.王社教、王会祥、谢增业、李梅，1992，塔里木盆地三套生油层成熟演化及成烃期的研究，见:塔里木盆地油气勘探论文集,童晓光、梁狄刚主编，乌每木齐:新.科技卫生出版社(K ),331-342。

    3.李术元、钱家麟、秦匡宗、朱亚杰，1987沥青作为中间产物的油页岩热解动力学的研究，姗料化学学报，15(2):118-123。
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  • Received:  1995-08-10
  • Published:  1995-12-10

Investigation on Secondary Generation of Hydrocarbons by Thermal Modelling of Kerogen

  • University of Petroleum, Beijing 102200
  • Received Date: 1995-08-10
  • Publish Date: 1995-12-10

Abstract: Based on results from thermal modelling experiments of kerogens,this paper presents a brief discussion on secondary generation of hydrocarbons. Geological effects, such as structural movement, etc.,may result in liftion or denudation of source rocks which do not enter highly-and post-mature phases, which causes the decrease of geotemperature of the source rocks and the cease of hydrocarbon generation. While the source rocks subside .again, the geotemperature increases, and when it reachs a certain point, the unexhaused kerogens may generate hydrocarbons again.The generated oil-gas amount with the continuous process of hydrocarbon generation is close to the total amounts of twice generations, indicating that hydrocarbon-generating amount is not affected by the secondary hydrocarbon generation that only defer generating oil and gas.

Liu Luofu, Wang Weihua, Li Shuyuan. Investigation on Secondary Generation of Hydrocarbons by Thermal Modelling of Kerogen[J]. Acta Sedimentologica Sinica, 1995, 13(S1): 147-150.
Citation: Liu Luofu, Wang Weihua, Li Shuyuan. Investigation on Secondary Generation of Hydrocarbons by Thermal Modelling of Kerogen[J]. Acta Sedimentologica Sinica, 1995, 13(S1): 147-150.
shu

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