世界核地质科学2024，Vol.41Issue(4)：756-764,9.DOI:10.3969/j.issn.1672-0636.2024.04.011
川西巴塘地区措纳柯温泉水成分及微量元素特征
Composition and trace element characteristics of Cuonake hot spring water in the Batang area of western Sichuan
摘要
Abstract
Hot springs are a precious resource for physical therapy and tourism,and their hydrochemical characteristics are of great significance for the evaluation and genesis research of thermal mineral water in physical therapy.The area where Cuonake hot spring islocated in Batang county,Sichuan province,has abundant tourism resources,and there are currently no detailed hydrochemical data reports on this hot spring.In order to help the development and utilization of Cuonake hot springs and the study of their genesis,this article collected representative hot spring water from Cuonake hot springs,conducted water quality measurement and trace element analysis,studied hydrochemical characteristics,conducted preliminary evaluation of physical therapy hot mineral water,and explored the genesis of the hot springs.The research results show that the temperature at the mouth of Cuonake hot spring is 50～65℃,and its hydrochemical type belongs to the HCO3-·Na type.The hot spring water has a high content of lithium,strontium,rubidium,cesium,tungsten,boron,fluorine,metasilicic and metaboric acid components.Among them,the fluorine,metasilicic acid,and metaboric acid content meet the concentration standards of medical value or named mineral water,making it a good physical therapy hot mineral water.The main utilization direction of hot springs is comprehensive utilization of physical therapy,health care,and heating.The thermal storage temperature of Cuonake hot spring ranges from 107.56 to 119.01℃(with an average of 114.30℃),and it belongs to a medium temperature geothermal resource of non magmatic heat source type.The atmospheric precipitation and melting water of ice and snow in the surrounding mountainous areas circulate along the nearly north-south trending fault zone and the northeast trending fault fracture zone to a higher temperature depth of about 3 300 m.They are heated by passing rocks and undergo strong water rock reactions with lithium rich granite,forming geothermal water rich in Li,Rb,Cs,B,Cl and other elements.Geothermal water rises along the fracture zone to form hot springs.关键词
水化学特征/理疗热矿水/成因/措纳柯温泉/川西巴塘地区Key words
hydrochemical characteristics/physical therapy hot mineral water/genesis/Cuonake hot spring/Batang area in western Sichuan分类
天文与地球科学引用本文复制引用
梅超,胡志华..川西巴塘地区措纳柯温泉水成分及微量元素特征[J].世界核地质科学,2024,41(4):756-764,9.基金项目
中核集团铀矿地质项目(编号:地GT2201) （编号:地GT2201）
核工业北京地质研究院院长青年科技创新基金项目(编号:热QJ2108)联合资助 Supported by CNNC Uranium Geological Project(No.地 GT2201) （编号:热QJ2108）
Youth Science and Technology Innovation Fund Project of Beijing Research Institute of Uranium Geology(No.热 QJ2108) （No.热 QJ2108）
