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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

季少聪 张庆玉 淡永 聂国权 闫剑飞 巴俊杰

中国地质2026,Vol.53Issue(1):77-92,16.
中国地质2026,Vol.53Issue(1):77-92,16.DOI:10.12029/gc20231026001

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

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

季少聪 1张庆玉 1淡永 2聂国权 1闫剑飞 2巴俊杰1

作者信息

  • 1. 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
  • 2. 中国地质调查局成都地质调查中心,四川 成都 610081
  • 折叠

摘要

Abstract

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.

关键词

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

Key words

shale gas/accumulation conditions/gas-bearing properties/Niutitang Formation/Well Guidudi 1/Southern Guizhou Depression/shale gas geological survey engineering

分类

天文与地球科学

引用本文复制引用

季少聪,张庆玉,淡永,聂国权,闫剑飞,巴俊杰..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[J].中国地质,2026,53(1):77-92,16.

基金项目

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). (桂科AB23026062)

中国地质

1000-3657

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