ISSN 1006-3021 CN11-3474/P
Published bimonthly started in 1979
滇东岩溶高原矿泉水类型及地质控制
  
关键词:eastern Yunnan  karst plateau  mineral water  classification characteristics  genetic types  countermeasures and suggestions
基金项目:国家重点研发计划专项(编号: 2016YFC0502502);中国地质调查局地质调查项目“滇西北地区生态地质调查”(编号: DD2019)
作者单位E-mail
张贵 云南省地质环境监测院 ynsghszg@163.com 
张华 云南省地质环境监测院  
王波 云南省地质环境监测院  
张文鋆 云南省地质环境监测院  
高瑜 云南省地质环境监测院  
何绕生 云南省地质环境监测院  
周翠琼 云南省地质环境监测院  
彭淑惠 云南省地质环境监测院  
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摘要:
Mineral Water Types and Geological Control in Karst Plateau of Eastern Yunnan
      The karst plateau area in eastern Yunnan has a complex stratigraphic structure and a complete range of outcropping rocks. The north belongs to the Upper Yangtze Platform and the south belongs to the South China Fold Belt. Geochemical processes and karstification processes have led to diverse types of mineral springs and abundant water resources. 363 water points consisting of various types of mineral springs have been discovered. Through investigation and summary, the mineral water in the area is classified into 6 types: metasilicic acid, salt, trace element, carbonic acid, compound type, and warm mineral water; according to the main controlling factors of formation conditions, the genetic types can be divided into 3 types: fault zone convection type, deep circulation stratification control type, and underflow leaching type. Karst has an impact on the formation of mineral water in eastern Yunnan, and can form characteristic strontium mineral water. The problems in development and utilization are summarized, and countermeasures and suggestions for optimal utilization of mineral water are put forward.
ZHANG Gui,ZHANG Hua,WANG Bo,ZHANG Wen-jun,GAO Yu,HE Rao-sheng,ZHOU Cui-qiong,PENG Shu-hui.2021.Mineral Water Types and Geological Control in Karst Plateau of Eastern Yunnan[J].Acta Geoscientica Sinica,42(3):333-340.
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