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武陵山地区下志留统石牛栏组狭缝型碳酸盐岩气成因分析

张婕 魏红霞 汪双清 沈斌 庞飞 李梦来 杨柳

中国地质2025,Vol.52Issue(2):691-703,13.
中国地质2025,Vol.52Issue(2):691-703,13.DOI:10.12029/gc20200928002

武陵山地区下志留统石牛栏组狭缝型碳酸盐岩气成因分析

Genesis analysis of slit-type carbonate gas reservoir in the Lower Silurian Shiniulan Formation in Wulingshan area

张婕 1魏红霞 1汪双清 1沈斌 1庞飞 2李梦来 3杨柳3

作者信息

  • 1. 国家地质实验测试中心,北京 100037
  • 2. 中国地质调查局,北京 100037
  • 3. 重庆地质矿产研究院,重庆 400042
  • 折叠

摘要

Abstract

This paper is the result of geological survey engineering. [Objective]Multiple sets of marine source rocks such as Cambrian-Ordovician,Silurian,Carboniferous-Permian,etc.are widely distributed in the northern Guizhou area of China,which have a good source-reservoir-caprock combination vertically and are of great natural gas resource potential and prospects for exploration and development.In order to better assess the natural gas resources in the area,on the basis of the discovery of the"four-story"composite natural gas reservoir in Anye 1 Well of the Anchang syncline in the Wulingshan area,northern Guizhou,this paper discusses the genesis of the Shiniulan Formation gas reservoir in the Anchang syncline.[Methods]Field geological works and indoor studies,geological probes and geochemical analyses,macroscopic observations and microscopic techniques,as well as literature researches were carried out.[Results]It is considered to be a slit-type carbonate gas reservoir,the gas is mainly derived from the underlying Longmaxi Formation,and the multiple stage tectonic movements in the area provided the driving force for its accumulation.[Conclusions]This research is significant for natural gas resources assessment of the region,and is also helpful for enriching and developing the theory of hydrocarbon accumulation in complex structural belts.

关键词

安页1井/石牛栏组/致密气/储集条件/地质调查工程

Key words

Anye 1 Well/Shiniulan Formation/tight gas/storage condition/geological survey engineering

分类

天文与地球科学

引用本文复制引用

张婕,魏红霞,汪双清,沈斌,庞飞,李梦来,杨柳..武陵山地区下志留统石牛栏组狭缝型碳酸盐岩气成因分析[J].中国地质,2025,52(2):691-703,13.

基金项目

国家科技重大专项(2016ZX05034-003)和中国地质调查局项目(DD20190086)联合资助. Supported by National Science and Technology Major Project(No.2016ZX05034-003)and China Geological Survey Project(No.DD20190086). (2016ZX05034-003)

中国地质

OA北大核心

1000-3657

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