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崂山花岗岩地区含锶、偏硅酸矿泉水的形成机理
引用本文:赵广涛,曹钦臣,孙悦鹏.崂山花岗岩地区含锶、偏硅酸矿泉水的形成机理[J].中国海洋大学学报(自然科学版),1996(2).
作者姓名:赵广涛  曹钦臣  孙悦鹏
摘    要:报道了崂山花岗岩地区矿泉水的特征。指出其矿泉类型为含锶、偏硅酸型,并讨论了其形成机理。

关 键 词:崂山花岗岩地区  含锶、偏硅酸矿泉水  形成机理

FORMATION MECHANISM OF STRONTIUM AND METASILICIC ACID-BEARING MINERAL WATER IN THE LAOSHAN MOUNTAIN GRANITOID AREA
Zhao Guangtao, Cao Qinchen, Sun Yuepeng.FORMATION MECHANISM OF STRONTIUM AND METASILICIC ACID-BEARING MINERAL WATER IN THE LAOSHAN MOUNTAIN GRANITOID AREA[J].Periodical of Ocean University of China,1996(2).
Authors:Zhao Guangtao  Cao Qinchen  Sun Yuepeng
Institution:Institute of Mineral Resources
Abstract:The characterisics of the mineral water in Laoshan Mountain granitic area are reported. The mineral water, with long term migration and lixiviation in the crevice of the rocks and forming in the dissolution - precipitation reaction between the granitic rocks and the underground water, is of Sr and metasilicic acid type. The forming inflencing factors of the mineral water include chemical composition of the mineral and the rocks, alteration degree of the rock infractur zone, time of the water-rock reaction, Co2 content in the water and run-off condition of the underground water, etc.
Keywords:Laoshan Mountain granitic area  Sr and H_2SiO_3-bearing mineral water  formation mechenism  
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