岩性油气藏 ›› 2025, Vol. 37 ›› Issue (5): 34–48.doi: 10.12108/yxyqc.20250504

• 地质勘探 • 上一篇    

鄂尔多斯盆地西缘奥陶系乌拉力克组页岩气勘探潜力

陆江1,2,3,4, 王健1,2,3, 吴楠1,2,3, 李程善5, 冯子飞6   

  1. 1. 长江大学 地球科学学院, 武汉 430100;
    2. 南方复杂页岩油气地质与开发湖北省重点实验室, 武汉 430100;
    3. 非常规油气地质与工程湖北省工程研究中心, 武汉 430100;
    4. 南方海洋科学与工程广东省实验室(湛江), 广东 湛江 524000;
    5. 中国石油长庆油田公司, 西安 710018;
    6. 中国石油长城钻探录井公司, 辽宁 盘锦 124010
  • 收稿日期:2025-05-14 修回日期:2025-06-09 发布日期:2025-09-06
  • 第一作者:陆江（1979—），男，博士，教授级高级工程师。主要从事石油与天然气地质方面的研究工作。地址:（430100）湖北省武汉市蔡甸区大学路111号。Email:lujiang@zjblab.com。
  • 通信作者: 王健（1992—），男，硕士，实验师。主要从事油气地球化学和油气成藏机理方面的研究工作。Email:wangjian2017@yangtzeu.edu.cn。
  • 基金资助:
    国家自然科学基金面上项目“鄂尔多斯盆地稳定克拉通背景下超压成因及其与演化过程”（编号：42172179）和南方复杂页岩油气地质与开发湖北省重点实验室开放基金“鄂尔多斯盆地安塞地区延长组7段陆相页岩油运移动力衰减机制”（编号：CGD-202402）联合资助。

Exploration potential of shale gas in Ordovician Wulalike Formation in the western margin of Ordos Basin

LU Jiang1,2,3,4, WANG Jian1,2,3, WU Nan1,2,3, LI Chengshan5, FENG Zifei6   

  1. 1. College of Geosciences, Yangtze University, Wuhan 430100, China;
    2. Hubei Key Laboratory of Complex Shale Oil and Gas Geology and Development in Southern China, Wuhan 430100, China;
    3. Hubei Engineering Research Center of Unconventional Petroleum Geology and Engineering, Wuhan 430100, China;
    4. Southern Marine Science and Engineering Guangdong Laboratory(Zhanjiang), Zhanjiang 524000, Guangdong, China;
    5. Changqing Oilfield Company, PetroChina, Xi'an 710018, China;
    6. GWDC Mud Logging Company, CNPC, Panjin 124010, Liaoning, China
  • Received:2025-05-14 Revised:2025-06-09 Published:2025-09-06

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摘要： 通过测井数据分析、矿物组分测试、扫描电镜分析、薄片观察、孔渗分析、氮气吸附测试和甲烷吸附测试等，对鄂尔多斯盆地西缘奥陶系乌拉力克组页岩储层开展了岩石学特征、物性及孔隙结构特征、生气潜力及含气性等研究。研究结果表明：①鄂尔多斯盆地西缘奥陶系乌拉力克组岩性以深灰—灰黑色泥页岩为主，分布稳定、厚度约78.9 m，矿物成分以石英为主，脆性矿物质量分数为70.98%～90.32%，脆性指数为50.03%～71.16%。②研究区页岩储层孔隙度普遍小于0.1%，渗透率普遍小于0.01 mD，孔隙类型主要为裂缝、纳米—微米级微孔和粒间溶孔，微观孔隙体积为0.016 27～0.033 73 cm3/g，以微孔和中孔为主。③研究区乌拉力克组页岩有机质类型主要为Ⅰ，Ⅱ1型，TOC最高为1.54%，有机质处于高成熟—过成熟阶段，在30℃时的甲烷最大吸附质量体积为0.99 m3/t，测井解释页岩气的质量体积最高为3.4 m3/t，与国内外典型优质页岩储层相比，其有机质丰度偏低，脆性矿物含量更高，含气量处于中等水平，具有较大的页岩气勘探潜力。

关键词: 页岩气, 脆性指数, 等温吸附实验, 微观孔隙结构, 高成熟—过成熟, 乌拉力克组, 奥陶系, 鄂尔多斯盆地西缘

Abstract: Combined with well logging data analysis，mineral composition testing，scanning electron microscopy analysis，thin section observation，pore permeability analysis，nitrogen adsorption testing，and methane adsorption testing，the research of petrological characteristics，physical properties，pore structure characteristics，gas potential，and gas-bearing properties of Ordovician Wulalike Formation shale reservoir in the western margin of Ordos Basin were conducted. The results show that：（1）Ordovician Wulalike Formation in the western margin of Ordos Basin is dominated by dark gray to gray black mud shale，these mud shales exhibit stable distribution and have a thickness of about 78.9 m. The mineral composition is mainly quartz，with a brittle mineral mass fraction of 70.98%-90.32% and a brittleness index of 50.03%-71.16%.（2）The porosity of shale reservoirs in the research area is generally less than 0.1%，and the permeability is generally less than 0.01 mD. The pore types are mainly fractures，nano-micron micropores，and intergranular dissolved pores. The microscopic pore volume is 0.016 27-0.033 73 cm3/g，mainly micropores and mesopores. （3）In the research area，main types of organic matter of Wulalike Formation shale are Type Ⅰ and Type Ⅱ1，and TOC can reach to 1.54%，the organic matter is in high maturity to over maturity stage，with a maximum methane adsorption mass volume of 0.99 m3/t under experimental conditions of 30 ℃. The highest shale gas mass volume in logging interpretation is 3.4 m3/t. Compared with typical high-quality shale reservoirs at home and abroad，its organic matter abundance is relatively low，the content of brittle minerals is relatively high，and the gas content is at a moderate level，indicating great potential for shale gas exploration.

Key words: shale gas, brittleness index, isothermal adsorption experiment, microscopic pore structure, high maturity to over maturity, Wulalike Formation, Ordovician, western margin of Ordos Basin

中图分类号: 

  • TE122
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