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河南范县地热资源地质特征及成矿机制分析

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河南范县地热资源区是河南省"十四五"地热资源找矿突破战略行动重要勘查区,具有分布面积广、水温高、涌水量和回灌率大等特点.通过对研究区地质背景和地热条件的分析研究,探求地热田的补给、径流和排泄途径,热储层地热流体赋存条件和成矿机理.结果表明:范县地热资源位于沉积盆地潜凸起型砂岩—岩溶二元热储地热田内;O-∈岩溶地热流体位于深循环—弱开放式环境;沉积盆地型地热田具有"四元"成矿机制分别为:一元为基底凸起区(隆起区),二元为构造影响带两侧,三元为新生界盖层(埋深1 200~1 500 m),四元为碳酸盐岩(灰岩、白云岩等)的基底.
Analysis of geological characteristics and metallogenic mechanism of geothermal resources of Fan County,Henan Province
The geothermal resource area in Fan County,Henan Province is an important exploration area for the"14th Five-Year Plan"geothermal resource prospecting breakthrough strategic action in Henan Prov-ince.This area is characterized by a wide distribution of high water temperature,large water inflow,and high recharge rate.Through the analysis of the geological background and geothermal conditions of the Fan County,the recharge,runoff and drainage paths of geothermal fields,the occurrence conditions and metallo-genic mechanism of geothermal fluids in geothermal reservoirs were investigated.The results show that the geothermal resources of Fan County are located in the geothermal field of the buried-uplift sandstone-karst binary geothermal reservoir in the sedimentary basin.The O-∈ karst geothermal fluid is located in a deep cir-culation-weak open environment.The sedimentary basin-type geothermal field has"four-elements"metallo-genic mechanism:one is the basement uplift area(uplift area),the binary is on both sides of the structural influence zone,the ternary is the cover layer of Cenozoic with a buried depth of 1 200 to 1 500 m,and the quaternary is the basement lithology of carbonate rock(limestone,dolomite,etc.).

geothermal resourcessedimentary basinkarst geothermal reservoirgeological characteristicsmetallogenic mechanismFan CountyHenan

卢磊、倪昆、刘亚南

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河南省国土空间调查规划院,河南郑州 450053

河南省地质局生态环境地质服务中心,河南郑州 450053

地热资源 沉积盆地 岩溶热储 地质特征 成矿机制 范县 河南

2024

矿产与地质
桂林矿产地质研究院

矿产与地质

CSTPCD
影响因子:0.42
ISSN:1001-5663
年,卷(期):2024.38(6)