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鄂尔多斯盆地神木气田太原组低品质气藏储层微观特征及形成机理

张涛 巩肖可 黄朝 曹青赟 孟凤鸣 董占民 陈朝兵 王恒力

石油实验地质2024,Vol.46Issue(1):32-45,14.
石油实验地质2024,Vol.46Issue(1):32-45,14.DOI:10.11781/sysydz202401032

鄂尔多斯盆地神木气田太原组低品质气藏储层微观特征及形成机理

Micro characteristics and formation mechanism of low-quality gas reservoirs in Taiyuan Formation of Shenmu Gas Field,Ordos Basin

张涛 1巩肖可 1黄朝 1曹青赟 1孟凤鸣 1董占民 1陈朝兵 2王恒力3

作者信息

  • 1. 中国石油天然气股份有限公司 长庆油田分公司 第二采气厂,西安 710200
  • 2. 西安石油大学 地球科学与工程学院,西安 710065||陕西省油气成藏地质学重点实验室,西安 710065
  • 3. 延安大学 石油工程与环境工程学院,陕西 延安 716000
  • 折叠

摘要

Abstract

Shenmu Gas Field in Ordos Basin shows the characteristics of low quality gas reservoir,and its deve-lopment effect is quite different from that of surrounding gas fields,which brings some problems to the exploration deployment and sustainable production of the gas field.In order to reveal the origin of low-quality gas reservoirs,the microscopic characteristics and formation mechanism of Taiyuan Formation reservoirs in Shenmu Gas Field were studied based on microscopic experiments at different scales.The results show that the reservoir of Taiyuan Formation in Shenmu Gas Field is characterized by"rich in quartz,poor in feldspar,and high content of rock detritus".The reservoir of Taiyuan Formation is a low porosity and ultra-low permeability tight sandstone reservoir with small pore-fine throat combination,poor pore throat connectivity,and weak reservoir permeability.The formation of low-quality reservoirs in Taiyuan Formation is affected by the matrix,the content of rock detritus in eruptive rocks and diagenesis.During the late Carboniferous to early Permian,the formation of the reservoir was significantly affected by the volcanic activity of the Inner Mongolia ancient uplift in the north of the Ordos Basin.The content of matrix and rock detritus of the eruptive rock in the sandstone was generally high.The rock detritus of the eruptive rock provided the main material basis for the development of secondary pores.While the matrix blocked the pores,it also produced a certain number of matrix dissolved pores,which had a dual impact on the reservoir.The dissolution during diagenesis is critical to the formation of Taiyuan Formation reservoir,and the increased porosity accounts for 64.3%of the current porosity.At the end of the Late Cretaceous,the late Yanshan movement led to the structural inversion of the Ordos Basin,the readjustment of gas and water,and the escape of natural gas along the fault in the eastern part of the basin.Finally,the low quality gas reservoir of Taiyuan Formation in Shenmu Gas Field is formed.The next exploration focus of Shenmu Gas Field should be based on the clear macro distribution law of diagenesis and favorable lithologic traps,and further search for the development area with high content of eruptive rock detritus and low content of matrix.

关键词

成岩作用/孔喉结构/凝灰质杂基/构造反转/太原组/神木气田/鄂尔多斯盆地

Key words

diagenesis/pore throat structure/tuffaceous matrix/structural inversion/Taiyuan Formation/Shenmu Gas Field/Ordos Basin

分类

能源科技

引用本文复制引用

张涛,巩肖可,黄朝,曹青赟,孟凤鸣,董占民,陈朝兵,王恒力..鄂尔多斯盆地神木气田太原组低品质气藏储层微观特征及形成机理[J].石油实验地质,2024,46(1):32-45,14.

基金项目

国家科技重大专项(2011ZX05044、2016ZX05050006)和中国石化科技攻关项目(P14150)联合资助. (2011ZX05044、2016ZX05050006)

石油实验地质

OA北大核心CSTPCD

1001-6112

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