贵州梵净山穹窿区地热资源赋存特征分析

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英文篇名：Analysis on the occurrence characteristics of geothermal resources in the Fanjing mountain dome region of Guizhou province 作者：吴小凤 ; 李军 英文作者：WU Xiaofeng;LI Jun;Guizhou Provincial Non-ferrous Metal and Nuclear Geological Exploration Bureau No.1 Battalion; 关键词：梵净山 ; 地热 ; 赋存特征 ; 贵州省 英文关键词：Fanjing mountain;;geothermal;;occurrence characteristics;;Guizhou province 中文刊名：中国矿业 英文刊名：China Mining Magazine 机构：贵州省有色金属和核工业地质勘查局一总队; 出版日期：2019-10-20 出版单位：中国矿业 年：2019 期：S2 语种：中文; 页：296-299 页数：4 CN：11-3033/TD ISSN：1004-4051 分类号：P314

摘要

梵净山穹窿区地热水呈带状分布,属中低温热矿水,其形成受区域性深大断裂控制。通过对梵净山穹窿区区域水文地质、地热地质条件研究,以及地热水成因分析,总结出梵净山穹窿区地热资源具有以下赋存特征:区域性断裂构造有带状热储形成条件;区域性断裂与背斜复合构造区具有地热田形成条件。梵净山属于世界自然遗产,旅游资源丰富,地热资源赋存条件较好,具有较高的开发利用价值。
        The geothermal water in the Fanjing mountain dome region distributes in zones and belongs to medium-low temperature hot mineral water.Its formation is controlled by regional deep and large faults.Based on the study of regional hydrogeology and geothermal geological conditions in Fanjing mountain dome area and the analysis of geothermal water genesis,it is concluded that the geothermal resources in Fanjing mountain area have the following characteristics:the formation conditions of zonal thermal reservoirs are in regional fault structures and the formation conditions of geothermal fields are in the composite structural areas of regional faults and anticlines.Fanjing mountain is a world natural heritage,rich in tourism resources,good conditions for geothermal resources,and has high value for development and utilization.

引文

[1]林日松，李军．江口县苗匡地热资源勘查报告[R].2017.
    [2]张学东，李军．印江县紫微地热资源勘查报告[R].2018.
    [3]张世从，陈履安．贵州热矿水[M]．贵阳：贵州科技出版社，1998.
    [4]谢配红．贵州印江峨岭地热勘查区地热地质条件及地热水特征浅析[J]．佳木斯职业学院学报，2016(9):489-491.XIE Peihong.Analysis of the feature of geothermal water and the condition of geothermal geological of geothermal exploration area of the Guizhou YinJiang ELing[J].Journal of Jiamusi Education Institute,2016(9):489-491.
    [5]国家质量监督检验检疫局．地热资源地质勘查规范：GB11615—2010[S]．北京：地质出版社，2010.