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歧口凹陷区新近系馆陶组热储特征及成因机制

夏国朝 楼达 赵艳婷 王辉 段忠丰 孙晓林 张飞鹏 雒蓉 葛家成

煤田地质与勘探2024,Vol.52Issue(1):46-55,10.
煤田地质与勘探2024,Vol.52Issue(1):46-55,10.DOI:10.12363/issn.1001-1986.23.10.0603

歧口凹陷区新近系馆陶组热储特征及成因机制

Characteristics and genetic mechanism of geothermal reservoirs in the Neogene Guantao Formation,Qikou Sag

夏国朝 1楼达 1赵艳婷 2王辉 1段忠丰 3孙晓林 2张飞鹏 1雒蓉 1葛家成1

作者信息

  • 1. 中国石油大港油田公司,天津 300280
  • 2. 天津地热勘查开发设计院,天津 300250
  • 3. 中国石油大学(华东) 地球科学与技术学院,山东 青岛 266580
  • 折叠

摘要

Abstract

The Qikou Sag in the Huanghua Depression,Bohai Bay Basin boasts extremely abundant geothermal re-sources.Among them,the geothermal reservoirs of the Neogene Guantao Formation have the greatest potential for ex-ploitation.To ascertain the properties of geothermal resources in this formation and rationally exploit these resources,it is significant to investigate the geothermal field,porosity,permeability,geothermal water circulation patterns,and genet-ic mode of geothermal reservoirs in the formation.Based on data from drilling,geophysical exploration,thermometry,and production of the study area,this study determined that the geothermal reservoirs of the Guantao Formation in the Qikou Sag constitute a conductive geothermal system of a sedimentary basin,with the heat flow from the deep mantle and the radioactive heat from the crust being transferred through heat conduction.The distribution of geothermal anom-alies is subjected to wavy bedrock.High-temperature geothermal anomalies with geothermal gradients up to above 5.0℃/hm are found near the Cangdong and Binhai faults.The geothermal reservoirs of the Guantao Formation manifest high porosity and permeability in the north and south but low porosity and permeability in the central portion,with porosity greater than 26% ,permeability above 390×10-3 μm2,and average single-well water yield of 60 m3/h overall.These suggest high-quality geothermal reservoirs.The geothermal water in the study area primarily originates from pa-leometeoric water.As the recharge source,the paleometeoric water from the Yanshan area in the north circulates deeply along strata while absorbing heat from the rock matrix,ultimately forming geothermal water.The geothermal reservoirs of the Guantao Formation in the Qikou Sag host geothermal resources of 41.81×1018 J,95% of which are distributed in the Tianjin Binhai New Area and Huanghua City,Hebei Province.Their high match with demands makes geothermal re-sources in the study area have great potential for production and utilization.

关键词

歧口凹陷/孔隙型热储/馆陶组/热储特征/成因模式/渤海湾盆地

Key words

Qikou Sag/porous geothermal reservoir/Guantao Formation/geothermal reservoir characteristics/genetic mode/Bohai Bay Basin

分类

天文与地球科学

引用本文复制引用

夏国朝,楼达,赵艳婷,王辉,段忠丰,孙晓林,张飞鹏,雒蓉,葛家成..歧口凹陷区新近系馆陶组热储特征及成因机制[J].煤田地质与勘探,2024,52(1):46-55,10.

基金项目

国家自然科学基金项目(42072130) (42072130)

中国石油天然气股份有限公司项目(2021DJ5501) (2021DJ5501)

煤田地质与勘探

OA北大核心CSTPCD

1001-1986

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