石油学报 ›› 2023, Vol. 44 ›› Issue (11): 1764-1780.DOI: 10.7623/syxb202311002

• 地质勘探 • 上一篇    下一篇

鄂尔多斯盆地东缘深部煤层气成藏演化规律与勘探开发实践

徐凤银1,2, 王成旺3,4, 熊先钺3, 徐博瑞1,3, 王红娜5, 赵欣6, 江山7, 宋伟8, 王玉斌3,4, 陈高杰3,4, 吴鹏1,3, 赵靖舟9   

  1. 1. 中联煤层气国家工程研究中心有限责任公司 北京 100095;
    2. 中国石油学会 北京 100724;
    3. 中石油煤层气有限责 任公司 北京 100028;
    4. 中石油煤层气有限责任公司工程技术研究院 陕西西安 710082;
    5. 中油油气勘探软件国家工程研究中心有限公司 北京 100080;
    6. 中国煤炭地质总局碳中和研究院 北京 100039;
    7. 长江大学地球科学学院 湖北荆州 434023;
    8. 中国石油青海油田公司 甘肃敦煌 736202;
    9. 西安石油大学地球科学与工程学院 陕西西安 710065
  • 收稿日期:2023-06-08 修回日期:2023-09-23 出版日期:2023-11-25 发布日期:2023-12-08
  • 通讯作者: 王成旺,男,1984年1月生,2011年获中国石油大学(华东)工学硕士学位,现为中石油煤层气有限责任公司高级工程师,主要从事煤层气、致密气地质工程一体化研究工作。Email:361883384@qq.com
  • 作者简介:徐凤银,男,1964年4月生,1993年获中国矿业大学工学博士学位,现为中联煤层气国家工程研究中心有限责任公司教授、博士生导师,中国石油学会副理事长兼秘书长,主要从事煤炭、煤层气、石油、天然气地质研究与管理工作。Email:xufy518@sina.com.cn
  • 基金资助:
    中国石油天然气股份有限公司攻关性应用性科技项目(2023ZZ18)和中石油煤层气有限责任公司科技项目(2021-KJ-04、2023-KJ-07)资助。

Evolution law of deep coalbed methane reservoir formation and exploration and development practice in the eastern margin of Ordos Basin

Xu Fengyin1,2, Wang Chengwang3,4, Xiong Xianyue3, Xu Borui1,3, Wang Hongna5, Zhao Xin6, Jiang Shan7, Song Wei8, Wang Yubin3,4, Chen Gaojie3,4, Wu Peng1,3, Zhao Jingzhou9   

  1. 1. China United Coalbed Methane National Engineering Research Center Co., Ltd., Beijing 100095, China;
    2. Chinese Petroleum Society, Beijing 100724, China;
    3. PetroChina Coalbed Methane Company Limited, Beijing 100028, China;
    4. Research Institute of Engineering Technology, PetroChina Coalbed Methane Company Limited, Shaanxi Xi'an 710082, China;
    5. CNPC Exploration Software Co., Ltd., Beijing 100080, China;
    6. Carbon Neutral Research Institute, China Administration of Coal Geology, Beijing 100039, China;
    7. School of Geosciences, Yangtze University, Hubei Jingzhou 434023, China;
    8. PetroChina Qinghai Oilfield Company, Gansu Dunhuang 736202, China;
    9. School of Earth Sciences and Engineering, Xi'an Petroleum University, Shaanxi Xi'an 710065, China
  • Received:2023-06-08 Revised:2023-09-23 Online:2023-11-25 Published:2023-12-08

摘要: 中国深部煤层气(埋深>1 500 m)资源丰富,具有吸附气与游离气共存的赋存特征,其赋存状态、成藏特征和开发规律与中—浅部煤层气存在显著差异,成藏演化规律尚不清晰制约了其高效勘探与开发。以鄂尔多斯盆地东缘大宁—吉县区块深部8号煤层为例,通过精细刻画深部煤层气的成藏特征,模拟深部煤层的埋藏演化史、热演化史、生烃演化史,完善了深部煤层气的富集成藏规律和成藏模式,并提出了针对性勘探开发对策。研究结果表明,大宁—吉县区块深部8号煤层全区发育、有机质热演化程度高、干酪根类型为Ⅲ型、生烃潜力大,总生烃强度为(20.2~34.7)×108m3/km2;深部煤储层发育割理、裂隙、组织孔、胞腔孔、气孔、晶间孔和溶蚀孔等储集空间,为深部游离态煤层气提供了良好的储集条件;构造-岩性-水动力耦合封闭利于深部煤层气保存。研究区深部煤层的成藏演化可以划分为初始生烃阶段(阶段Ⅰ,306~251 Ma)、第1次热成因生烃阶段(阶段Ⅱ,251~203 Ma)、有机质热演化作用减缓阶段(阶段Ⅲ,203~145 Ma)、生烃高峰阶段(阶段Ⅳ,145~130 Ma)和成藏状态定型阶段(阶段Ⅴ,130 Ma至今)5个阶段。研究区深部煤层气表现为游离态与吸附态共存,提出了深部煤层气"广覆式生烃、箱式封闭、微构造调整、自生自储、毯式成藏"的富集成藏规律,建立了微幅褶皱与物性耦合控藏(Ⅰ型)、微幅单斜与水动力耦合控藏(Ⅱ型)、物性与水动力耦合控藏(Ⅲ型)3类深部煤层气成藏模式。研究认识有效指导了大宁—吉县区块深部煤层气勘探有利区的优选,建立了深部煤储层有利区评价指标体系,针对不同成藏模式发育区,提出了差异化开发方案,助力研究区实现了深部煤层气真正意义上的效益开发。研究认识对于中国其他区块开展深部煤层气勘探与开发具有重要参考与借鉴意义。

关键词: 深部煤层气, 成藏演化, 成藏模式, 成藏条件, 鄂尔多斯盆地, 开发技术对策

Abstract: China's deep coalbed methane (CBM) resources, with the burial depths exceeding 1 500 m, are abundant and coexist with adsorbed and free gases. The occurrence state, accumulation characteristics, and development laws of deep CBM differ significantly from those of mid-shallow CBM, and the unclear evolution patterns have restricted its efficient exploration and development. Taking the No.8 deep coal seam in Daning-Jixian block on the eastern margin of Ordos Basin for example, this study finely characterizes the accumulation characteristics of deep CBM and simulates the burial evolution history, thermal evolution history, and hydrocarbon generation history of deep coal seams, thus improving the deep CBM enrichment and accumulation laws and patterns; moreover, the targeted exploration and development strategies are proposed. The results show that the No.8 deep coal seam is widespread in Daning-Jixian block, with high organic matter thermal maturity and Type III kerogen. This indicates significant hydrocarbon generation potential, with the total hydrocarbon intensity of (20.2-34.7) ×108m3/km2. The deep coal reservoir develops cleats, fractures, texture pores, cell pores, gas pores, intergranular pores, and dissolution pores, providing favorable conditions for the accumulation of deep free-state CBM. The structural-lithologic-hydrodynamic coupling closure is favorable for the preservation of deep CBM. The evolution stages of hydrocarbon accumulation in deep coal seams in the study area include the initial hydrocarbon generation stage (Stage I, 306-251 Ma), the first thermal hydrocarbon generation stage (Stage II, 251-203 Ma), the decreasing stage of organic matter thermal evolution (Stage III, 203-145 Ma), the hydrocarbon generation peak stage (Stage IV, 145-130 Ma), and the final formation stage of the oil/gas accumulation pattern (Stage V, 130 Ma to present). The deep CBM under free and adsorbed states coexist in the study area. On this basis, the paper proposes the hydrocarbon enrichment and accumulation pattern of "wide covering hydrocarbon generation, box-type closure, microstructure adjustment, self-generation and self-storage, and blanket-type accumulation", and establishes three types of deep CBM accumulation models:microfold and physical property coupling control (Type I), microfault monocline and hydrodynamic force coupling control (Type II), and physical property and hydrodynamic force coupling control (Type III) on reservoir accumulation. These understandings can effectively guide the selection of favorable areas for deep CBM exploration in Daning-Jixian block, establish an evaluation index system for favorable areas in deep coal reservoirs, propose differentiated development plans for exploration areas with different accumulation models, and help achieve the truly efficient and low-cost development of deep CBM in the study area. The research findings have important reference significance for carrying out deep CBM exploration and development in other blocks in China.

Key words: deep coalbed methane, accumulation and evolution, accumulation model, accumulation conditions, Ordos Basin, development technology strategies

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