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现代地质 ›› 2022, Vol. 36 ›› Issue (04): 998-1008.DOI: 10.19657/j.geoscience.1000-8527.2021.194

• 油气勘探 • 上一篇    下一篇

基于包裹体信息分析准噶尔盆地柴窝堡凹陷芦草沟组储层油源及成藏期次

郑瑞辉1,2(), 金霄1,2, 郑铎1,2,3, 李佳阳1,2, 陈雪1,2, 张枝焕1,2()   

  1. 1.中国石油大学(北京) 地球科学学院,北京 102249
    2.中国石油大学(北京) 油气资源与探测国家重点实验室,北京 102249
    3.中国石化胜利油田分公司 孤岛采油厂,山东 东营 257015
  • 收稿日期:2021-02-10 修回日期:2021-04-15 出版日期:2022-08-10 发布日期:2022-09-09
  • 通讯作者: 张枝焕
  • 作者简介:张枝焕,男,教授,博士生导师,1962年出生,有机地球化学专业,主要从事有机地球化学研究。Email: zhangzh3996@vip.163.com
    郑瑞辉,男,博士研究生,1991年出生,石油地质学专业,主要从事有机地球化学研究。Email: zhengrh2016@163.com

Inclusion Data Analysis for the Determination of Oil Source and Accumulation Stages in Lucaogou Formation in the Chaiwopu Sag, Junggar Basin

ZHENG Ruihui1,2(), JIN Xiao1,2, ZHENG Duo1,2,3, LI Jiayang1,2, CHEN Xue1,2, ZHANG Zhihuan1,2()   

  1. 1. College of Geoscience, China University of Petroleum, Beijing 102249, China
    2. State Key Laboratory of Petroleum Resources and Prospecting, China University of Petroleum,Beijing 102249, China
    3. Gudao Oil Production Plant, Shengli Oilfield Company, SINOPEC, Dongying, Shandong 257015, China
  • Received:2021-02-10 Revised:2021-04-15 Online:2022-08-10 Published:2022-09-09
  • Contact: ZHANG Zhihuan

摘要:

柴窝堡凹陷芦草沟组原油的研究工作取得了重要进展,但由于构造沉积演化十分复杂,目前油源方面的认识仍不清楚,成藏时间尚不明确。利用改进的石油包裹体烃组分分析方法和包裹体定年技术讨论了研究区芦草沟组原油的来源和成藏期次。结果表明,研究区芦草沟组储层第一期充注原油正构烷烃主峰碳数低,C21三环萜烷和C27甾烷相对丰度较高,显示蓝色荧光,为北部半深湖—深湖相芦草沟组烃源岩生成的高成熟原油,于早白垩世在达1井区聚集成藏;第二期充注原油正构烷烃主峰碳数高,C20三环萜烷或C23三环萜烷、C29甾烷相对丰度较高,显示黄绿色、黄色荧光,为研究区滨浅湖相芦草沟组烃源岩生成的较低成熟度原油,于晚白垩世末期—古新世早期在达1井区聚集成藏。

关键词: 柴窝堡凹陷, 包裹体烃组分, 油气来源, 成藏期次, 油气成藏过程

Abstract:

Hydrocarbon accumulation in the Chaiwopu Sag has been well documented, however the tectonic and sedimentary evolution in the Chaiwopu Sag is complex, and the source of oil and the timing of hydrocarbon accumulation are still controversial. Here, the hydrocarbon source and accumulation of the Lucaogou Formation is discussed through an improved molecular composition of inclusion method, and the fluid inclusions in the Chaiwopu Sag (Junggar Basin). Distribution characteristics of the n-alkanes are dominated by low carbon numbers, and the relative abundance of C21-tricyclic terpane and C27-steranes are higher in the early-charging oil, showing blue fluorescence. The first stage (Early Cretaceous) oil came mainly from the Lucaogou Formation (semi-)deep lacustrine-facies source rocks in the north. Meanwhile, distribution characteristics of the n-alkanes are dominated by high carbon numbers, and the relative abundance of C20-tricyclic terpane or C23-tricyclic terpane and C29-steranes are higher in the second-charging oil, showing yellow-green or yellow fluorescence. The second stage lasted from the end Late Cretaceous to the Early Paleocene, and the oil came mainly from the local Lucaogou Formation shore-shallow lacustrine-facies source rocks.

Key words: Chaiwopu Sag, inclusion molecular composition, hydrocarbon source, hydrocarbon accumulation period, hydrocarbon accumulation process

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