摘要
Abstract
According to the mineralization conditions of the mineral water,the fluorine limit and the circulation depth of the mineral water produced in the bedrock weathering shell and secondary structural belt,the relationship between the water temperature and the circulation depth of the mineral water,and the previous summary and analysis of exploration depth of the source area of the mineral water,It is believed that the mineral water in southern China is mainly of metasilicate acid type with low salinity,most of which are shallow circulation groundwater,and the depth of minerogenic circulation is mostly in the range of tens of meters to one or two hundred meters,under the general natural environmental conditions,most of the circulation can be metallogenic within a few months to one or two years,and in rapid cases.it can be metallogenic in the groundwater of the year or the season.It is of practical significance to fully understand the essential characteristics of depth and time of mineralization circulation of mineral water in southern China,summarize the location and depth rules conducive to the formation and occurrence of the mineral water,guide exploration and prospecting of the mineral water,guide mineral water enterprises to exploit reasonably and pay attention to the environmental protection of water source.关键词
天然矿泉水/偏硅酸型/浅循环/短期/成矿Key words
Natural mineral water/Metasilicate acid type/Shallow circulation/Short-term/Metallogenic分类
天文与地球科学
