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蜀南地区下二叠统孔洞型碳酸盐储层特征

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四川盆地蜀南地区下二叠统碳酸盐岩储层具有重要的天然气资源潜力.本文通过对蜀南地区栖霞组和茅口组的储层特征进行详细分析,揭示了下二叠统碳酸盐岩储层的岩石类型、储集空间和储层物性特征.研究结果表明,蜀南地区的储集岩主要包括微生物粘结灰岩、颗粒灰岩和白云岩.其中,栖霞组的储集岩主要为喀斯特改造的微生物粘结灰岩,次为白云岩;茅口组则以颗粒灰岩为主,其次为白云岩.储集空间主要分为孔隙、洞穴和裂缝.孔隙度和渗透率数据表明,栖霞组和茅口组普遍表现为低孔低渗特征,部分区域存在较高孔隙度的段位.尽管下二叠统白云岩储层的地质资料不足,相关数据仍显示白云岩孔隙度普遍高于其他岩石类型,表明其具有较好的储集性能.本研究为蜀南地区下二叠统的勘探开发提供了重要的储层基础.
Features of cavity-type carbonate reservoirs in the Lower Permian of the southern Sichuan region
The Lower Permian carbonate reservoirs in the southern Sichuan region exhibit significant natural gas resource potential.This study provides a detailed analysis of the reservoir characteristics in the Qixia and Maokou formations of the southern Sichuan region,revealing the rock types,storage spaces,and reservoir physical properties of the Lower Per-mian carbonates.The results indicate that the primary reservoir rocks in the region include microbial binding limestone,granular limestone,and dolomite.Among these,the Qixia for-mation predominantly consists of microbial binding limestone modified by karst processes,followed by dolomite.The Maokou formation is primarily composed of granular limestone,with dolomite as a secondary component.The storage spaces are mainly classified into pores,caves,and fractures.Data on porosity and permeability reveal that both the Qixia and Maokou formations generally exhibit low porosity and low permeability characteristics,with some ar-eas showing higher porosity segments.Although geological data for the Lower Permian dolomite reservoirs are limited,available data suggest that the porosity of dolomite is gener-ally higher than that of other rock types,indicating superior reservoir performance.This study provides a crucial foundation for the exploration and development of the Lower Permi-an reservoirs in the southern Sichuan region.

biogenic limestonedolomiteporosity typesstorage space

何洋

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中国石油集团川庆钻探工程公司地质勘探开发研究院,四川 成都 610051

生物灰岩 白云岩 孔隙类型 储集空间

2024

石油化工应用
宁夏化工学会

石油化工应用

影响因子:0.276
ISSN:1673-5285
年,卷(期):2024.43(11)