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鄂尔多斯盆地上古生界致密砂岩储层微观孔隙特征

于波

西安科技大学学报2018,Vol.38Issue(1):150-155,6.
西安科技大学学报2018,Vol.38Issue(1):150-155,6.DOI:10.13800/j.cnki.xakjdxxb.2018.0121

鄂尔多斯盆地上古生界致密砂岩储层微观孔隙特征

Micro-characteristics of Upper Paleozoic tight reservoir of Ordos Basin

于波1

作者信息

  • 1. 陕西延长石油(集团)有限责任公司,陕西 西安710075
  • 折叠

摘要

Abstract

Gas resources in Upper Paleozoic tight reservoir,Ordos Basin are rich,which as an important complement resource,is gaining more and more attention.By obersving cores,identifying casting lamel-la,scanning electron microscope and mercury porosimetry technique,the special micro-pore structure of tight-sand reservoir was researched.A contrastive analysis of the effect on pore characteristics by differ-ent kind of diagenesis was carried out. The results show that: four types of pores are intergranular pores,dissolved intra-grain pores,intercrystalline pores,and micro-fractures develop in Ordos Basin. The main pore type of He 8 and Shan 1 is dissolved intra-grain pores and intercrystalline pores while that of Shan 2 is intergranularpores.Those three types of diagenesis have great influences on pore-char-acteristics with compaction rendering most while dissolution least.Great compaction leads to a high lev-el of reservoir micro-pore.

关键词

地质资源与地质工程/鄂尔多斯盆地/上古生界/微观孔隙结构特征/成岩作用

Key words

geological resources and geological engineering/Ordos Basin/Upper Paleozoicerathem/mi-cro-pore structure/diagenesis

分类

能源科技

引用本文复制引用

于波..鄂尔多斯盆地上古生界致密砂岩储层微观孔隙特征[J].西安科技大学学报,2018,38(1):150-155,6.

基金项目

国家科技重大专项(2012KTZ03-03-01-01) (2012KTZ03-03-01-01)

西安科技大学学报

OA北大核心CSTPCD

1672-9315

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