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摘要:
The geothermal water hydrochemistry and isotopic characteristics of boreholes in the Suijiang-1 well in Yunnan Province were studied based on the actual drilling geology, regional geological structure and hydrogeological conditions. The analysis results show that the geothermal water is SO4-Ca·Mg type, the recharge elevation is 1 381-1 646 m, the recharge source is atmospheric precipitation, the geothermal reservoir temperature is 42-45 ℃, and the geothermal water is controlled by lithology and geological structure conditions of study area. Atmospheric precipitation enters the groundwater circulation system through the surface karst form of the Wujiaobao anticline, northwest-southeast tensile faults, fissures and karst depression, and geothermal water formed through the rising deep cycle water temperature, then blocked by the double rivers’ fault zone and drilling explosion.
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篇名 Geological characteristics and analysis of hydrothermal genesis in the Suijiang-1 well in Yunnan 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 water HYDROCHEMISTRY Origin ANALYSIS of hot spring
年,卷(期) dxskxygcywb_2019,(1) 所属期刊栏目
研究方向 页码范围 53-60
页数 8页 分类号 TV
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GEOTHERMAL
water
HYDROCHEMISTRY
Origin
ANALYSIS
of
hot
spring
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研究去脉
引文网络交叉学科
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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
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0
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