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吐哈盆地十三间房地区煤系烃源岩生烃评价及排烃特征

吴志远 彭苏萍 杜文凤

吴志远, 彭苏萍, 杜文凤. 吐哈盆地十三间房地区煤系烃源岩生烃评价及排烃特征[J]. 矿业科学学报, 2016, 1(2): 103-112.
引用本文: 吴志远, 彭苏萍, 杜文凤. 吐哈盆地十三间房地区煤系烃源岩生烃评价及排烃特征[J]. 矿业科学学报, 2016, 1(2): 103-112.
Wu Zhiyuan, Peng Suping, Du Wenfeng. Evaluation of the hydrocarbon generation and hydrocarbon expulsion characteristics of coal-measure source rock in Shisanjianfang area,Tuha Basin[J]. Journal of Mining Science and Technology, 2016, 1(2): 103-112.
Citation: Wu Zhiyuan, Peng Suping, Du Wenfeng. Evaluation of the hydrocarbon generation and hydrocarbon expulsion characteristics of coal-measure source rock in Shisanjianfang area,Tuha Basin[J]. Journal of Mining Science and Technology, 2016, 1(2): 103-112.

吐哈盆地十三间房地区煤系烃源岩生烃评价及排烃特征

基金项目: 国家重点研发计划课题(2016YFC0501102)
国家科技重大专项课题(2016ZX05066-001)
国家自然科学基金煤炭联合项目(U1261203)
详细信息
    作者简介:

    吴志远(1987—),男,河南信阳人,博士研究生,主要从事煤系烃源岩评价、油气盆地模拟方面的研究。

  • 中图分类号: TE122.1

Evaluation of the hydrocarbon generation and hydrocarbon expulsion characteristics of coal-measure source rock in Shisanjianfang area,Tuha Basin

  • 摘要: 利用钻井、地震数据及三维地质建模技术对十三间房地区煤系烃源岩厚度及分布特征进行了预测,根据地球化学测试数据对十三间房地区水西沟群烃源岩的有机质类型、有机质丰度、有机质成熟度进行了评价,利用生烃潜力法建立了研究区烃源岩的排烃模式,明确了研究区的排烃特征.研究结果表明,研究区西北部烃源岩厚度较大,在350~600m之间,平均值为480m.烃源岩有机质丰度较高,处于成熟—高成熟热演化阶段,有机质类型主要为Ⅱ、Ⅲ类,具有一定的生烃潜力.研究区水西沟群煤岩排烃门限深度为2000m,最大排烃率为530mg/g,在2500m处迅速达到排烃高峰,最大排烃速率为150mg/(g·hm);煤系泥岩排烃门限深度为2200m,在2800m处迅速达到排烃高峰,最大排烃率为320mg/g,表明研究区具有一定的开采潜力.本次研究对相似地质条件地区生烃和排烃研究具有一定的借鉴意义.
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出版历程
  • 收稿日期:  2016-05-13
  • 刊出日期:  2016-10-29

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