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摘要:
In general, previous geothermal geochemical studies in Guangdong Province mainly involves single method to cover limited aspects and areas. In that way, various methods available cannot actually provide more convincing results of geothermal fluid’s circulation system and evolution process from different dimensions, especially in terms of isotope. As a result, more comprehensive researches remain to be done on geochemistry of geothermal fluid, in particular, the space-time law of isotope’s evolution pattern as well as recharge cycle. Based on data of environmental isotopes (2H and 18O) and the isotope of radiometric dating (14C), geothermal geology, characteristics of groundwater flow field and types of goethermal reservior in Guangdong Province are taken into account in this paper, so as to analyze numerical rule and spatial distribution features of isotopes. Thus, corresponding main causes, mechanism and hydrogeological significance can be revealed to further study the potential of geothermal fluid to renew and recharge in the long run, which is conducive to enrich geothermal theories and solve existing hydrogeological problems.
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篇名 Research on basic characteristics of 2H, 18O and 14C in geothermal fluid in Guangdong Province, China
来源期刊 地下水科学与工程:英文版 学科 工学
关键词 GEOTHERMAL FLUID ISOTOPE CHARACTERISTICS TYPES of GEOTHERMAL reservior
年,卷(期) dxskxygcywb_2019,(1) 所属期刊栏目
研究方向 页码范围 42-52
页数 11页 分类号 TV
字数 语种
DOI
五维指标
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研究主题发展历程
节点文献
GEOTHERMAL
FLUID
ISOTOPE
CHARACTERISTICS
TYPES
of
GEOTHERMAL
reservior
研究起点
研究来源
研究分支
研究去脉
引文网络交叉学科
相关学者/机构
期刊影响力
地下水科学与工程:英文版
季刊
2305-7068
河北省石家庄市中华北大街268号
出版文献量(篇)
277
总下载数(次)
0
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