摘要
两个研究区所处大地构造环境相似,其热矿水大多属于含氮硅质热水,忻州盆地一些热水是东亚大陆上一种新的水化学类型的热水:SO_4-Cl-Na-Ca水,对比已经开发利用多年的贝加尔裂谷带医疗矿水,忻州盆地热水中锶、有机碳、环烷酸等含量普遍较高,具有较高的矿泉治疗学价值,贝加尔裂谷带热水化学成分复杂多样;这与其所处地质-水文地质条件密切相关。
The geothermal mineral waters in the Xinzhou Basin and Baikal Rift Zone,located in tectonically similar environments,are N2-bearing siliceous thermal fluids. The hydrochemi-cal type of some thermal waters in Xinzhou ,i. e. SO4-Cl-Na-Ca water,is recognized for the first time on the East Asia continent. As compared with the mineral waters in the Baikal Rift Zone which have been applied in medical practice for many years,the relatively high contents of strontium, organic carbon and naphthenic acids of thermal waters in Xinzhou determine their relatively high value for their future medical application. The chemical compositions of the thermal waters in Baikal are variable and complex, which are closely related with the local geologic-hydrogeologic conditions.
出处
《地球科学（中国地质大学学报）》
EI
CAS
CSCD
北大核心
1993年第5期661-670,共10页
Earth Science-Journal of China University of Geosciences
关键词
矿水
水化学
可溶性
有机物质
裂谷
mineral water ,hydrochemistry,soluble organic matter , biologically active components ,graben,rift zone.
