首页|期刊导航|中国地质|黔南坳陷贵都地1井下寒武统牛蹄塘组页岩含气性及其影响因素研究

黔南坳陷贵都地1井下寒武统牛蹄塘组页岩含气性及其影响因素研究OA

Research on gas content and its influencing factors of shale gas of the Lower Cambrian Niutitang Formation in Well Guidudi 1,southern Guizhou Depression

中文摘要英文摘要

[研究目的]雪峰隆起西南缘下寒武统牛蹄塘组是目前上扬子地区页岩气勘探的重点领域,本文旨在查明该区牛蹄塘组页岩气聚集条件及含气特征,明确页岩气富集主控因素.[研究方法]以最新部署的贵都地 1井钻井及测试分析资料为基础,对牛蹄塘组富有机质页岩的岩石学特征、有机地球化学特征、储层物性、储集空间类型及含气性特征进行深入研究,对比分析牛蹄塘组一段与三段页岩气聚集主控因素及差异.[研究结果](1)牛蹄塘组一段页岩矿物成分以脆性矿物为主,占 66.14%.牛蹄塘组三段页岩黏土矿物、脆性矿物、碳酸盐矿物含量均衡,分别占 36.45%、33.09%、30.45%;(2)牛蹄塘组一段页岩TOC平均值为 4.71%,有机质类型属Ⅰ型,Ro平均值为3.59%.牛蹄塘组三段页岩TOC平均值为 2.20%,有机质类型属Ⅰ型,Ro平均值为 3.18%;(3)共识别出粒内溶孔、粒间孔、晶间孔、有机孔和微裂缝 5种储集空间类型,牛蹄塘组一段以有机孔、粒间孔、微裂缝为主,牛蹄塘组三段以粒内溶孔为主;(4)牛蹄塘组三段现场解析总含气量平均值为 1.03 m3/t,牛蹄塘组一段现场解析总含气量平均值为 0.22 m3/t.[结论]通过对比牛蹄塘组一段与三段页岩气聚集条件和含气性,牛蹄塘组一段页岩气聚集主要受有机质丰度、矿物成分、孔隙结构等条件的影响,含气量与有机碳含量、碎屑矿物含量呈正相关,牛蹄塘组三段页岩气聚集主要受矿物成分、储集空间等条件的影响,含气量与碳酸盐矿物含量呈正相关.

This paper is the result of shale gas geological survey engineering. [Objective]The Niutitang Formation of the Lower Cambrian in the southwestern margin of the Xuefeng Uplift is currently a key area for shale gas exploration in the Upper Yangtze region.This study aims to identify the accumulation conditions and gas-bearing properties of shale gas in the Niutitang Formation of the research area,and to clarify the main controlling factors for shale gas enrichment.[Methods]Based on the newly deployed drilling and testing analysis data of Well Guidudi 1,the petrological characteristics,organic geochemical characteristics,reservoir physical properties,reservoir space types and gas bearing properties of organic shale in the Niutitang Formation have been thoroughly studied.The main controlling factors and differences in shale gas accumulation in the first and third sections of the Niutitang Formation have been compared and analyzed.[Results](1)The mineral composition of the shales in the Niutitang Formation Section 1 is mainly brittle minerals,accounting for 66.14%.The contents of clay minerals,brittle minerals,and carbonate minerals of the shales in the Niutitang Formation Section 3 are balanced,accounting for 36.45%,33.09%,and 30.45%,respectively;(2)The average TOC value of the shale in the Niutitang Formation Section 1 is 4.71%,and the organic matter type belongs to type Ⅰ,with an average Ro value of 3.59%.The average TOC value of the shale in the Niutitang Formation Section 3 is 2.20%,and the organic matter type belongs to type Ⅰ,with an average Ro value of 3.18%;(3)Five types of reservoir spaces are identified,including intragranular dissolved pores,intergranular pores,intergranular pores,organic pores,and microcracks.The Niutitang Formation Section 1 is mainly composed of organic pores,intergranular pores,and microcracks,while the Niutitang Formation Section 3 is mainly composed of intragranular dissolved pores;(4)The average total gas content analyzed on site in the Niutitang Formation Section 3 is 1.03 m3/t.The average total gas content analyzed on site in the Niutitang Formation Section 1 is 0.22 m3/t.[Conclusions]By comparing the accumulation conditions and gas content of shale gas in the first and third sections of the Niutitang Formation,it is found that the accumulation of shale gas in the Niutitang Formation Section 1 is mainly influenced by conditions such as organic matter abundance,mineral composition,and pore structure.The gas content is positively correlated with organic carbon content and detrital mineral content.The accumulation of shale gas in the Niutitang Formation Section 3 is mainly influenced by conditions such as mineral composition and storage space,and the gas content is positively correlated with carbonate mineral content.

季少聪;张庆玉;淡永;聂国权;闫剑飞;巴俊杰

中国地质科学院岩溶地质研究所/自然资源部、广西岩溶动力学重点实验室/联合国教科文组织国际岩溶研究中心,广西 桂林 541004||广西平果喀斯特生态系统国家野外科学观测研究站,广西 平果 531406中国地质科学院岩溶地质研究所/自然资源部、广西岩溶动力学重点实验室/联合国教科文组织国际岩溶研究中心,广西 桂林 541004||广西平果喀斯特生态系统国家野外科学观测研究站,广西 平果 531406中国地质调查局成都地质调查中心,四川 成都 610081中国地质科学院岩溶地质研究所/自然资源部、广西岩溶动力学重点实验室/联合国教科文组织国际岩溶研究中心,广西 桂林 541004||广西平果喀斯特生态系统国家野外科学观测研究站,广西 平果 531406中国地质调查局成都地质调查中心,四川 成都 610081中国地质科学院岩溶地质研究所/自然资源部、广西岩溶动力学重点实验室/联合国教科文组织国际岩溶研究中心,广西 桂林 541004||广西平果喀斯特生态系统国家野外科学观测研究站,广西 平果 531406

天文与地球科学

页岩气聚集条件含气性牛蹄塘组贵都地1井黔南坳陷页岩气地质调查工程

shale gasaccumulation conditionsgas-bearing propertiesNiutitang FormationWell Guidudi 1Southern Guizhou Depressionshale gas geological survey engineering

《中国地质》 2026 (1)

77-92,16

广西重点研发计划项目(桂科AB23026062)、中国地质科学院岩溶地质研究所基本科研业务费项目(2022011、2023004)、中国地质调查局项目(DD20221658)和广西自然科学基金项目(2022GXNSFBA035454)联合资助. Supported by Guangxi Key Research and Development Program Project(No.AB23026062),Basic Research Expenses of Institute of Karst Geology,CAGS(No.2022011,No.2023004),the project of China Geological Survey(No.DD20221658)and Guangxi Natural Science Foundation(No.2022GXNSFBA035454).

10.12029/gc20231026001

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