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关中盆地新近系蓝田-灞河组热储层物性及渗流特征研究

张莹 任战利 兰华平 祁凯 邢光远 夏岩

地质通报2024,Vol.43Issue(5):712-725,14.
地质通报2024,Vol.43Issue(5):712-725,14.DOI:10.12097/gbc.2022.12.015

关中盆地新近系蓝田-灞河组热储层物性及渗流特征研究

Physical properties and percolation characteristics of Neogene Lantian-Bahe Formation thermal reservoir in Guanzhong Basin

张莹 1任战利 2兰华平 1祁凯 1邢光远 1夏岩3

作者信息

  • 1. 西北大学大陆动力学国家重点实验室,陕西西安 710069||西北大学地质学系,陕西西安 710069
  • 2. 西北大学大陆动力学国家重点实验室,陕西西安 710069||西北大学地质学系,陕西西安 710069||西安市多种能源资源勘探开发重点实验室,陕西西安 710069
  • 3. 中国石油长庆油田分公司勘探开发研究院,陕西西安 710018||低渗透油气田勘探开发国家工程实验室,陕西西安 710018
  • 折叠

摘要

Abstract

Guanzhong Basin is rich in geothermal resources,and its development and utilization will help to adjust the energy structure,reduce haze and improve the environment.The Neogene Lantian-Bahe Formation is the main stratum exploited at present.It is of great significance for effective development and reinjection of geothermal energy to clarify reservoir physical properties and seepage mechanism.Through core data and logging data,combined with mercury injection,casting thin section,nuclear magnetic resonance and other related testing methods,the physical property,pore structure and seepage characteristics of the Neogene Lantian-Bahe Formation in the Weihe Basin are analyzed in detail.The results show that:①The porosity in the plane of Lantian Bahe Formation is 7%~30%,with an average of 15%;permeability changes greatly,0.05~5689 mD,generally more than 30 mD.②The pores of Lantian-Bahe Formation are mainly primary intergranular pores and intergranular residual pores,with a small amount of microcracks and feldspar dissolution pores can be seen locally.The pore throat distribution is relatively uniform,mainly between 10 and 16 μm.The contribution value of permeability is high.The water yield can reach 80 m3/h,and the unit water inflow of sandstone with unit thickness can reach 0.0035 m3/(h·m2)with good water yield and seepage characteristics.③The reservoir type of Lantian-Bahe Formation belongs to Class Ⅱreservoir,which is comprehensively evaluated as high porosity permeable layer,and is the most favorable geothermal development interval.

关键词

热储层/孔隙结构/渗流/蓝田-灞河组/地热资源/关中盆地

Key words

thermal reservoir/pore structure/seepage/Lantian-Bahe Formation/geothermal resources/Guanzhong Basin

分类

天文与地球科学

引用本文复制引用

张莹,任战利,兰华平,祁凯,邢光远,夏岩..关中盆地新近系蓝田-灞河组热储层物性及渗流特征研究[J].地质通报,2024,43(5):712-725,14.

基金项目

国家重点研发计划《未固结砂岩热储层保护与增效钻完井技术及材料》专题《不同地区典型未固结砂岩热储层特征及评价》(编号:2019YFB1504201-01)、长庆油田分公司勘探开发研究院合作项目《关中盆地地热资源调查及开发技术政策研究》 (编号:2019YFB1504201-01)

地质通报

OA北大核心CSTPCD

1671-2552

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