中国石油勘探 ›› 2025, Vol. 30 ›› Issue (3): 75-88.DOI: 10.3969/j.issn.1672-7703.2025.03.006

• 石油地质 • 上一篇    下一篇

柴达木盆地上石炭统和中侏罗统煤岩气地质特征与勘探方向

刘国勇1,张永庶1,薛建勤1,龙国徽1,2,马峰3,王波1,王永生1,张长好1,周飞1,田继先4,孙秀建3,吴志雄1   

  1. 1 中国石油青海油田公司;2 中国地质大学(北京);3 中国石油勘探开发研究院西北分院;4 中国石油勘探开发研究院
  • 出版日期:2025-05-15 发布日期:2025-05-15
  • 作者简介:刘国勇(1978-),男,湖北荆州人,博士,2007年毕业于中国石油大学(北京),教授级高级工程师,主要从事油气田地质勘探综合研究与管理工作。地址:甘肃省敦煌市七里镇中国石油青海油田公司,邮政编码:736202。
  • 基金资助:
    中国石油天然气股份有限公司科技项目“柴达木盆地风险勘探领域和目标研究、工程技术攻关及现场试验”(2023YQX10108)。

Geological characteristics and exploration orientations of the Upper Carboniferous and Middle Jurassic coal rock gas in Qaidam Basin

Liu Guoyong1,Zhang Yongshu1,Xue Jianqin1,Long Guohui1,2,Ma Feng3,Wang Bo1, Wang Yongsheng1,Zhang Changhao1,Zhou Fei1,Tian Jixian4,Sun Xiujian3,Wu Zhixiong1   

  1. 1 PetroChina Qinghai Oilfield Company; 2 China University of Geosciences (Beijing); 3 PetroChina Research Institute of Petroleum Exploration & Development–Northwest; 4 PetroChina Research Institute of Petroleum Exploration & Development
  • Online:2025-05-15 Published:2025-05-15

摘要: 野外露头和钻井揭示柴达木盆地普遍发育古生界—中生界煤岩,具备一定的生烃潜力和良好储集性能,是盆地全新的勘探领域,但研究认识程度较低。通过对柴达木盆地中生界中侏罗统大煤沟组和古生界上石炭统克鲁克组煤岩沉积环境、煤岩分布、煤质特征、煤岩储层特征及煤岩气资源量和富集规律等方面开展系统研究,评价了柴达木盆地的煤岩气资源潜力,提出了勘探部署方向。研究表明:(1)中侏罗统湖沼相煤岩单层厚度为 2~30m,分布面积达11100km2;上石炭统海陆过渡相煤岩单层厚度为1~6m,分布面积为5689km2。(2)中侏罗统和上石炭统煤岩为半光亮—光亮煤,达到中煤阶演化阶段,均具有生气能力;中侏罗统大煤沟组煤岩TOC为32.22%~79.50%,平均为62.85%,Ro为0.77%~1.38%,平均为0.9% ;上石炭统克鲁克组煤岩TOC为35.67%~98.34%,平均为72.40%,Ro为 0.92%~1.82%,平均为1.57%。(3)煤岩储层孔渗性能好,割理密度高,呈网状分布,连通性好;气孔、铸模孔、溶蚀孔、晶间孔和植物组织孔等基质孔隙发育;煤岩实测孔隙度达5.26%~34.01%,平均为15.65% ;渗透率为5.11~12.60mD,平均为8.91mD。(4)纵向上发育5种煤岩气聚散组合,其中广泛分布的煤岩—泥岩与煤岩—石灰岩聚气组合,封闭条件好,录井全烃气测峰值高,是煤岩气富集的最佳组合。(5)优选柴达木盆地北缘圆顶山—九龙山地区中侏罗统和德令哈地区都兰—乌兰地区上石炭统有利区作为首选勘探战略部署区带。上述认识以期指导柴达木盆地煤岩气战略部署,开辟煤岩气勘探新领域,揭开盆地天然气勘探新篇章。

关键词: 柴达木盆地, 煤岩气, 上石炭统, 中侏罗统, 煤岩储层, 富集条件

Abstract: Field outcrops and drilling data reveal that the Paleozoic–Mesozoic coal rocks are widely distributed in Qaidam B asin, with certain hydrocarbon generation potential and good reservoir performance, which is a new exploration field in the basin. However, the level of research and understanding is relatively low. A systematic study on coal rocks in the Middle Jurassic Dameigou Formation and the Upper Carboniferous Keluke Formation in Qaidam Basin is conducted, including sedimentary environment, distribution, coal properties, reservoir characteristics, resource amount, and gas enrichment rules. In addition, gas resource potential in coal rocks is evaluated, and exploration deployment orientations are proposed in Qaidam Basin. The study results show that: (1) The limnic facies coal rocks in the Middle Jurassic have a single layer thickness of 2 – 30 m and a distribution area of 11100 km2; The transitional facies coal rocks in the Upper Carboniferous have a single layer thickness of 1 – 6 m and a distribution area of 5689 km2. (2) The coal rocks in the Middle Jurassic and the Upper Carboniferous are semi-bright to bright coals in a middle coal rank stage, all possessing gas generation capacity; TOC of coal rocks in the Middle Jurassic Dameigou Formation is 32.22%–79.50%, with an average of 62.85%, and Ro is 0.77%–1.38%, with an average of 0.9%; TOC of coal rocks in the Upper Carboniferous Keluke Formation is 35.67%–98.34%, with an average of 72.40%, and Ro ranges in 0.92%–1.82%, with an average of 1.57%. (3) The coal rock reservoirs are characterized by good porosity and permeability properties, and the coal cleats have a high density, showing a reticular distribution pattern and good connectivity; The matrix pores such as stomata, mold pores, dissolution pores, intercrystal pores and plant tissue pores are observed; The measured porosity of coal rocks ranges from 5.26% to 34.01%, with an average of 15.65%; The permeability is 5.11–12.60 mD, with an average of 8.91 mD. (4) Five types of gas accumulation and dispersion combinations are classified vertically in coal rocks, among which the widely distributed coalrock–mudstone and coal rock–limestone gas accumulation combinations have good sealing conditions and high peak values of total hydrocarbon gas logging shows, indicating the most favorable combinations for coal rock gas enrichment. (5) The favorable areas of the Middle Jurassic in Yuandingshan–Jiulongshan area in the northern margin of Qaidam Basin and the Upper Carboniferous in Dulan–Wulan in Delingha area are optimally selected for further strategic exploration deployment. The above understanding is expected to guide the strategic deployment of coal rock gas in Qaidam Basin, open up a new field for coal rock gas exploration, and unveil a new chapter in natural gas exploration in the basin.

Key words: Qaidam Basin, coal rock gas, Upper Carboniferous, Middle Jurassic, coal rock reservoir, gas enrichment condition

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