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作 者:宰西 黄建国[1] 马浩翔 徐世光[2] 杨壮 ZAI Xi;HUANG Jian-guo;MA Hao-xiang;XU Shi-guang;YANG Zhuang(Plateau Mountain Spatial Information Survey Technique Application Engineering Research Center at Yunnan Province’s Universities,Kunming 650093,China;Yunnan Bureau of Geology and Mineral Exploration and Development,Kunming 650200,China)
机构地区:[1]昆明理工大学国土资源工程学院,昆明650093 [2]云南省地质矿产勘查开发局(云南省地质矿产局),昆明650200
出 处:《地质灾害与环境保护》2021年第3期86-91,共6页Journal of Geological Hazards and Environment Preservation
摘 要:云南西部陇川县勐约乡研究区小范围内出露地热泉,该区地热成因及地热田范围并不明确,地热成因争议较大。本文以勐约地热田为研究对象,结合前人研究成果和区内地热钻井资料并在此基础上开展了对地热成因分析,在盖层、热源、热储和热通道等要素方面对该区地热条件、地温场特征、地热形成机理进行研究,构建地热地质成因模型。综合分析认为:(1)水化学类型为HCO_(3)^(-)~Na^(+)型水;(2)该区地热田热源主要来源于上地幔的岩浆,高热岩浆囊构成本区主要热源。In the research area of Mengyue Township,Longchuan County,western Yunnan Province,geothermal springs are found in a small area.The scope of geothermal genesis and geothermal field in this area is not clear,and the geothermal genesis is controversial.This paper takes Mengyue geothermal field as the research object,combines previous research results and geothermal drilling data in the area,and carries out geothermal genesis analysis on the basis of this.The geothermal conditions,characteristics of geothermal field and geothermal formation mechanism in this area were studied in terms of cover layer,heat source,heat storage and heat channel,and the geological genetic model of geothermal was constructed.The comprehensive analysis shows that:(1)the hydrochemical type is HCO_(3)^(-)~Na^(+) water;(2)the heat source of the geothermal field is mainly from the magma of the upper mantle,and the high hot magma sac is the main heat source in this area.
分 类 号:P314.1[天文地球—固体地球物理学]
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