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川东南志留系龙马溪组页岩储层微孔隙结构及连通性研究

刘伟新 鲍芳 俞凌杰 张文涛 张庆珍 卢龙飞 范明

石油实验地质2016,Vol.38Issue(4):453-459,7.
石油实验地质2016,Vol.38Issue(4):453-459,7.DOI:10.11781/sysydz201604453

川东南志留系龙马溪组页岩储层微孔隙结构及连通性研究

Micro-pore structure and connectivity of the Silurian Longmaxi shales, southeastern Sichuan area

刘伟新 1鲍芳 2俞凌杰 1张文涛 2张庆珍 1卢龙飞 2范明1

作者信息

  • 1. 中国石化 石油勘探开发研究院 无锡石油地质研究所,江苏 无锡 214126
  • 2. 中国石化 油气成藏重点实验室,江苏 无锡 214126
  • 折叠

摘要

Abstract

Micro⁃pore structure and connectivity of the Silurian Longmaxi shales in the southeastern Sichuan Basin were studied using CT, FIB-SEM, Ar+-SEM, and TEM techniques. Four modes for micro⁃pores in shales were de⁃termined to be as follows. (1) Intergranular micro⁃pores which exist between mineral grains and account for a small proportion of the total. (2) Intragranular micro⁃pores which mainly exist in intergranular dispersed organic matter or symbiosis organic matter with globular pyrite, and some between clay layers. (3) Grain boundary fractures which exist around organic or mineral grains, and work as a connective network for the shales. (4) Interlayer bedding which provides filtration channels. Intraparticle organic nano⁃pores are bubble like, show a normal size distribu⁃tion, and are connected to each other. Their diameter mainly ranges from 30-90 nm and throat width ranges from 7-20 nm. Interlayer bedding accounts for 1%-2% of total shale pores and fractures, and are favorable filtration channels. Micro⁃pores and fractures in organic matter provide the main reservoir space for shale gas, grain boundary fractures form a connective network, while interlayer bedding provides filtration channels.

关键词

孔隙结构/储集空间/渗滤通道/页岩/龙马溪组/志留系/川东南

Key words

pore structure/connectivity/reservoir space/filtration channel/shales in Longmaxi Formation/southeastern Sichuan Basin

分类

能源科技

引用本文复制引用

刘伟新,鲍芳,俞凌杰,张文涛,张庆珍,卢龙飞,范明..川东南志留系龙马溪组页岩储层微孔隙结构及连通性研究[J].石油实验地质,2016,38(4):453-459,7.

基金项目

国家自然科学基金项目(41372130)和中国石化科技部项目(P13089)资助。 ()

石油实验地质

OA北大核心CSCDCSTPCD

1001-6112

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