摘要
小娘坑矿区铁矿、水泥用灰岩矿属矽卡岩型铁矿,矿区属可溶岩岩溶矿山,矿区岩溶发育率约11.9%。矿区岩溶发育受可溶岩岩性特征和构造发育特征控制较显著,岩溶在水平、垂直空间上发育具由一定的发育特征。
Xiaoniangkeng iron mine and cement limestone mine belong to skarn type iron mine,and the mine belongs to karst mine with karst development rate of about 11.9%.The karst development in the mining area is obviously controlled by the characteristics of the lithology and structure of the soluble rock,and the karst development has certain characteristics in the horizontal and vertical space.
作者
边林浩
BIAN Lin-hao(The eighth Geological Brigade of Fujian Province,Longyan 364012,China)
出处
《化工管理》
2021年第14期80-81,共2页
Chemical Engineering Management
关键词
小娘坑矿区
可溶的岩岩性
岩溶发育特征
Xiaoniangkeng mining area
soluble rock lithology
karst development characteristics
