首页|期刊导航|西安石油大学学报(自然科学版)|黔西南下石炭统旧司组页岩气富集条件及其控制因素

黔西南下石炭统旧司组页岩气富集条件及其控制因素OA

Enrichment Conditions of Shale Gas in Lower Carboniferous Jiusi Formation in Southwestern Guizhou and Their Controlling Factors

中文摘要英文摘要

为明确黔西南下石炭统旧司组页岩气富集特征及控制因素,以下石炭统旧司组为研究对象,选取不同沉积相带的调查井,综合运用场发射扫描电镜、覆压孔渗、X-射线衍射、有机地球化学、现场解析及高压等温吸附等试验手段,系统分析了页岩气富集地质特征,探讨有机碳含量、有机质成熟度、矿物组分、岩相、孔渗特征及埋深等控制因素.结果表明:黔西南旧司组泥页岩沉积厚度介于 50~150 m,有机质丰度中等(平均1.68%),有机质类型以Ⅱ1、Ⅱ2 型为主,处于高成熟—过成熟早期阶段,具备良好的页岩气富集物质基础;旧司组页岩主要造岩矿物为石英和黏土矿物,脆性指数较高(平均51.75%),储层受沉积相控制,岩相以含黏土硅质页岩、含硅黏土质页岩为主,其中硅质页岩相、含黏土硅质页岩相为有利岩相;TOC含量与含气量呈正相关,比表面积、含气量与石英质量分数呈正相关,与碳酸盐矿物质量分数呈负相关.研究认为,有机质丰度、岩石矿物组分及埋深是影响黔西南旧司组页岩气富集的主要控制因素,有利岩相及较高脆性指数为页岩气储集与改造提供了有利条件.

To clarify the enrichment characteristics and controlling factors of the Lower Carboniferous Jiusi Formation shale gas in southwestern Guizhou,the geological characteristics of the Lower Carboniferous Jiusi Formation shale gas enrichment of the investigation wells in different sedimentary facies belts were systematically analyzed by means of the experimental methods including field emission scanning electron microscopy(FESEM),overburden pressure porosity and permeability test,X-ray diffraction(XRD),organic geo-chemistry analysis,on-site desorption,and high-pressure isothermal adsorption,and the controlling factors of the Lower Carboniferous Ji-usi Formation shale gas enrichment such as total organic carbon(TOC)content,organic matter maturity,mineral composition,lithofa-cies,porosity-permeability characteristics,and burial depth are discussed.The results show that:the muddy shale of the Jiusi Forma-tion in southwestern Guizhou has a large sedimentary thickness(50~150 m),moderate organic matter abundance(with an average of 1.68%),mainly type Ⅱ1 andⅡ2 organic matter,and is in the high-maturity to early over-maturity stage,providing a good material ba-sis for shale gas enrichment.The main rock-forming minerals of the Jiusi Formation shale are quartz and clay minerals,with high brittle-ness index(average51.75%).The shale reservoir is controlled by sedimentary facies,and the lithofacies are dominated by clay-bear-ing siliceous shale and silica-bearing argillaceous shale,among which the clay-bearing siliceous shale facies is favorable lithofacies.TOC content is positively correlated with gas content,the specific surface area and gas content are positively correlated with the mass fraction of quartz but negatively correlated with the mass fraction of carbonate mineral.It is held that organic matter abundance,rock mineral composition,and burial depth are the main controlling factors of the shale gas enrichment in the Jiusi Formation of southwestern Guizhou,and the favorable lithofacies and high brittleness index provide favorable conditions for shale gas storage and reservoir reconstruction.

李凯;周国正;高为;黄元庭;何勇;易明军;张栋;彭真

贵州省煤层气页岩气工程技术研究中心,贵州 贵阳 550008||贵州省煤田地质局一五九队,贵州盘州 561600||贵州省能源智能开发与高效利用实验室,贵州 贵阳 550008贵州省煤田地质局一五九队,贵州盘州 561600贵州省煤层气页岩气工程技术研究中心,贵州 贵阳 550008||贵州省煤田地质局一五九队,贵州盘州 561600||贵州省能源智能开发与高效利用实验室,贵州 贵阳 550008||贵州大学资源与环境工程学院,贵州 贵阳 550025贵州盘江精煤股份有限公司,贵州盘州 553536贵州盘江精煤股份有限公司火烧铺矿,贵州盘州 561600贵州盘江精煤股份有限公司火烧铺矿,贵州盘州 561600贵州省能源局,贵州 贵阳 550008贵州省能源局,贵州 贵阳 550008

天文与地球科学

页岩气富集特征控制因素旧司组下石炭统黔西南

shale gasenrichment characteristicscontrolling factorsJiusi FormationLower Carboniferoussouthwestern Guizhou

《西安石油大学学报(自然科学版)》 2026 (2)

12-23,12

贵州省科技计划项目(黔科合战略找矿[2022]ZD005、黔科合平台KXJZ[2025]055、黔科合支撑[2025]一般062)

10.3969/j.issn.1673-064X.2026.02.002

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