新疆石油地质 ›› 1995, Vol. 16 ›› Issue (4): 307-311.

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塔里木盆地轮台断隆带中新生代陆相原油成因及其源岩潜力评价

张水昌, 邓攀, 彭燕, 徐志明, 李梅, 肖中尧, 阎刚   

  1. 中国石油天然气总公司 石油勘探开发科学研究院 北京 100083
  • 收稿日期:1995-05-31 出版日期:1995-12-01 发布日期:2021-01-15
  • 作者简介:张水昌 高级工程师 石油地质

ORIGIN OF MESOZOIC-CENOZOIC CONTINENTAL FACIES OIL AND HYDROCARBON-GENERATED POTENCIAL EVALUATION OF SOURCE ROCK, LUN-TAI FAULTED UPLIFT ZONE IN TARIM BASIN

Zhang Shuichang, Deng Pan, Peng Yan, Xu Zhiming, Li Mei, Xiao Zhongyuan, Yan Gang   

  1. Scientifit Research Insti-tute of Petroleum Exploration and Development, CNPC, Beijing 100083
  • Received:1995-05-31 Online:1995-12-01 Published:2021-01-15
  • About author:Zhang Shuichang, Senior Engineer,Petroleum Geology

摘要: 通过油一油、油一岩地球化学性质对比后认为,轮台断隆带中西段原油来自库车坳陷三叠系黄山街组湖相泥岩地层,东段原油来自同一坳陷侏罗系湖沼相煤系地层。该两套岩系均具有相当高的生油潜力。

关键词: 塔里木盆地, 轮台断隆带, 库车生油坳陷, 侏罗纪, 三叠纪, 地层, 生油潜力评价

Abstract: On the basis of correlation of geochemical characteristics of oil-oil and oil-source rock, it is considered that oil in the middle and western parts of Luntai faulted up-lift zone was generated from lacustrine mudstone of Huangshanjie formation (Triassic) in Kuqa depression, and oil in the eastern part was from limnetic coal measure of Jurassic in Kuqa depression, which have extremely high hydrocarbon-generated potencial.

Key words: Tarim basin, Luntai faulted uplift zone, Kuqa depression, Jurassic, Triassic, Strata, Source rock evaluation