岩性油气藏 ›› 2023, Vol. 35 ›› Issue (4): 16–28.doi: 10.12108/yxyqc.20230402

• 地质勘探 • 上一篇    下一篇

准噶尔盆地西部坳陷二叠系下乌尔禾组烃源岩生烃潜力评价

唐勇1, 王智强2, 庞燕青3, 邓世坤3, 王超2, 洪鹏辉4   

  1. 1. 中国石油新疆油田公司, 新疆 克拉玛依 834000;
    2. 中国石油新疆油田公司 采油二厂, 新疆 克拉玛依 834000;
    3. 中国石油新疆油田公司 评价处, 新疆 克拉玛依 834000;
    4. 北京奥能恒业能源技术有限公司, 北京 100089
  • 收稿日期:2022-11-16 修回日期:2023-03-24 出版日期:2023-07-01 发布日期:2023-07-01
  • 第一作者:唐勇(1967-),男,博士,教授级高级工程师,主要从事盆地地质综合研究及风险勘探方面的工作。地址:(834000) 新疆克拉玛依市中国石油新疆油田公司勘探开发研究院。Email:tyong@petrochina.com.cn。
  • 通信作者: 洪鹏辉(1987-),男,硕士,工程师,主要从事石油地质与勘探方面的研究工作。Email:hongpenghui@126.com。
  • 基金资助:
    中国石油天然气股份有限公司前瞻性基础性研究重大科技项目“准噶尔盆地二叠系全油气系统地质理论与勘探实践”（编号：2021DJ0108）、“页岩油富集规律、资源潜力与有利区带目标评价研究”（编号：2021DJ1801）和中国石油天然气股份有限公司重大科技项目“陆相中高成熟度页岩油勘探开发关键技术研究与应用”（编号：2019E-26）资助。

Hydrocarbon-generating potential of source rocks of Permian lower Urho Formation in western depression，Junggar Basin

TANG Yong1, WANG Zhiqiang2, PANG Yanqing3, DENG Shikun3, WANG Chao2, HONG Penghui4   

  1. 1. PetroChina Xinjiang Oilfield Company, Karamay 834000, Xinjiang, China;
    2. No. 2 Oil Production Plant, PetroChina Xinjiang Oilfield Company, Karamay 834000, Xinjiang, China;
    3. Department of Reservoir Evaluation, PetroChina Xinjiang Oilfield Company, Karamay 834000, Xinjiang, China;
    4. Beijing Aonenghengye Energy Technology Co., Ltd., Beijing 100089, China
  • Received:2022-11-16 Revised:2023-03-24 Online:2023-07-01 Published:2023-07-01

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摘要： 利用岩石热解、镜下观察、热演化史分析、生烃热模拟实验及盆地模拟等手段，从岩性、有机质特征、生物标志物特征、规模有效烃源灶的分布特征等方面对准噶尔盆地西部坳陷二叠系下乌尔禾组烃源岩的生烃潜力进行了系统研究。研究结果表明： ①西部坳陷下乌尔禾组烃源岩主要为一套纹层不明显的泥岩沉积，岩性包括深灰色泥岩、灰色粉砂质泥岩、灰色泥质粉砂岩及灰色含炭粉砂质泥岩等，局部颜色深。②下乌尔禾组烃源岩整体生烃潜力一般且样品间差异性明显，有机质类型主要为Ⅲ型干酪根，岩石热解氢指数HI一般小于100 mg/g，为倾气型烃源岩；有机质成熟度分布范围大，镜质体反射率Ro为0.64%～1.56%，平均1.06%，产率指数PI为0.05～0.74，平均0.33，总体位于主生油窗，现今沙湾凹陷、盆1井西凹陷和玛湖凹陷分别处在生油高峰晚期、生凝析油/湿气和生干气阶段；有机质丰度、生烃潜力差别大，TOC值为0.29%～9.16%，平均0.85%，生烃潜量（S1+S2）为0.29～3.16 mg/g，平均0.74 mg/g，样品中差烃源岩和中等—好烃源岩各占50%。③下乌尔禾组烃源岩以浅湖沉积为主，处于淡水、弱氧化环境，以陆源有机质输入为主，几乎无碳酸盐输入，岩性、沉积环境均与风城组烃源岩差异大，生烃潜力更小。④下乌尔禾组烃源岩生烃中心为盆1井西凹陷，发育规模大，其中烃源岩厚度大于100 m的区域面积达16 000 km2，生烃强度大于500×104 t/km2的烃源岩分布面积达6 800 km2，具备形成大中型油气田的资源潜力。

关键词: 生烃潜力, 烃源岩, 生烃热模拟, 下乌尔禾组, 二叠系, 西部坳陷, 准噶尔盆地

Abstract: The hydrocarbon-generating potential of Permian lower Urho Formation source rocks in western depression of Junggar Basin were systematically studied from lithology，organic matter characteristics，biomarker characteristics and distribution characteristics of large-scale effective hydrocarbon source stoves by means of RockEval pyrolysis，microexamination，thermal evolution analysis，thermal simulation experiment of hydrocarbon generation and basin modeling. The results show that：（1）The source rocks of lower Urho Formation in western depression are mainly mudstone deposits with inconspicuous laminae，and the lithologies include dark grey mudstone， grey silty mudstone，grey argillaceous silty mudstone，and grey carbonaceous silty mudstone.（2）The source rocks of lower Urho Formation have hydrocarbon-generating potential and its differences of samples is obvious， and the organic matters are mainly composed of type Ⅲ kerogen with the Rock-Eval hydrogen index（HI）generally less than 100 mg/g，which indicates a set of gas-prone source rocks. The maturities of organic matters vary widely with the vitrinite reflectance（Ro）ranging from 0.64% to 1.56%（1.06% on average）and the production index （PI）ranging from 0.05 to 0.74（0.33 on average）. At present，the source rocks in Shawan，Pengyijingxi and Mahu sags are in the late oil-generating-peak，condensate/wet-gas-generating stage，and dry-gas-generating stage，respectively. The abundance and hydrocarbon-generating potential vary greatly with the TOC ranging from 0.29% to 9.16%（0.85% on average）and S1+S2 ranging from 0.29 to 3.16 mg/g（0.74 mg/g on average），respectively. Poor and medium-good source rocks account for 50% of the total samples respectively.（3）The source rocks of lower Urho Formation were deposited in fresh-oxidized environment，mainly with terrigenous organic matter input and almost no carbonate input. The lithology and sedimentary environment are different from that of the source rocks of Fengcheng Formation，and the hydrocarbon generation potential is lower.（4）The hydrocarbon generation center of the source rocks of lower Urho Formation is located in western well Pen-1 sag，which has a large development scale. The area of the source rocks with a thickness greater than 100 m is 16 000 km2， and the area of the source rocks with a hydrocarbon generation intensity greater than 500×104 t/km2 is 6 800 km2，showing a favorable potential to form large and medium-sized oil and gas fields.

Key words: hydrocarbon-generating potential, source rock, thermal simulation of hydrocarbon generation, lower Urho Formation, Permian, western depression, Junggar Basin

中图分类号: 

  • TE122.1
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