桃源县矿区地下水同位素特征分析  

Analysis of isotopic characteristics of groundwater in Taoyuan mining area

作　　者：欧阳波罗 刘声凯 赵凯[1] OUYANG Bo-luo(Team 416,Hunan Geological and Mineral Exploration and Development Bureau,Changsha 410000,China)

机构地区：[1]湖南省地质矿产勘查开发局四一六队,湖南长沙410000

出　　处：《世界有色金属》2020年第10期200-201,共2页World Nonferrous Metals

摘　　要：自从上世纪50年代以来,同位素技术开始用于水文地质学领域的研究,解决了一些水文地质学中的研究问题。近些年来,随着同位素分析技术的发展,同位素技术得到了进一步的应用和发展,尤其是在追踪地下水的补给过程、查明地下水起源、判断地下水的年龄方面有着深厚的应用基础。本文通过同位素特征来查明地下桃源县热市镇地下热水的来源。Since the 1950s,isotope technology has been used in the field of hydrogeology and solved some problems in hydrogeology.In recent years,with the development of isotope analysis technology,isotope technology has been further applied and developed,especially in tracking the recharge process of groundwater,identifying the origin of groundwater,and determining the age of groundwater.In this paper,the source of underground hot water in Reshi town of underground Taoyuan County was identified by isotopic characteristics.

关 键 词：氘氧同位素 锶同位素 地下热水成因 

分 类 号：P641[天文地球—地质矿产勘探]