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四川盆地灯影组储层特征及主控因素

斯春松 郝毅 周进高 倪超 潘立银

成都理工大学学报(自然科学版)Issue(3):266-273,8.
成都理工大学学报(自然科学版)Issue(3):266-273,8.DOI:10.3969/j.issn.1671-9727.2014.03.02

四川盆地灯影组储层特征及主控因素

Characteristics and controlling factors of reservoir in Sinian Dengying Formation,Sichuan Basin,China

斯春松 1郝毅 2周进高 3倪超 3潘立银3

作者信息

  • 1. 中国地质大学 资源学院,武汉 430074
  • 2. 中国石油杭州地质研究院,杭州 310023
  • 3. 中国石油杭州地质研究院,杭州 310023
  • 折叠

摘要

Abstract

Dengying Formation of Sinian is one of the most important gas-bearing strata in Precambrian of China.Based on the lithology characteristics,the scanning electron microscope,the cathode luminescence and some other experimental analyses,this paper studies some samples taken from the outcrops and the drilling cores of Dengying Formation in Sichuan Basin.This paper studies the dolomite reservoir of Dengying Formation.The types of the dolomite reservoir are mainly the algal stromatolite dolomite,algal lamellar dolomite,algal dolarenite,algal oncolite dolomite and algal grumous dolomite,and so on.There are altogether 6 kinds of reservoir pore spaces in Dengying Formation.Among them,the interbreccia pores,the mass dissolved pores-caves and the “grape-lace”remnant pores-caves are very important.The Development of the dolomite reservoir is mainly controlled by sedimentary facies,dolomitization,dissolution,sea level ecstasy and tectonic action. The sedimentary facies is the environment basement of the reservoir.The dolomization is the key that the reservoir can be preserved.The dissolution,sea level eustasy and tectonic action are the key factors to make pore spaces.The tectonic fracture is an important factor to improve the reservoir.The cementation and silicification will fill the pores and are destructive factors for the reservoir in Dengying Formation.

关键词

四川盆地/震旦系/灯影组/白云岩储层/控制因素

Key words

Sichuan Basin/Sinian/Dengying Formation/dolomite reservoir/controlling factor

分类

能源科技

引用本文复制引用

斯春松,郝毅,周进高,倪超,潘立银..四川盆地灯影组储层特征及主控因素[J].成都理工大学学报(自然科学版),2014,(3):266-273,8.

基金项目

国家科技重大专项(2011ZX05004-002);中国石油勘探与生产分公司前期研究项目 ()

成都理工大学学报(自然科学版)

OA北大核心CSCDCSTPCD

1671-9727

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