摘要
安乡硅土矿床赋存于地洼余动期亚构造层中,矿石主要由粉石英、伊利石和蒙脱石组成,是一个具有很好开发应用前景的大型非金属矿床。
The Anxiang siliceous earth depesit is located in the substructural layer of Diwa recidual-mobility period. The ore is mainly composed of quartz,illite and montmorillonite. It is a large-scale monmetallic deposit and has vety good exploiting prospect.
出处
《大地构造与成矿学》
EI
CAS
CSCD
1996年第2期184-187,共4页
Geotectonica et Metallogenia
基金
湖南省计委科研计划(省院合作)资助
关键词
洞庭地洼
石英
伊利石
蒙脱石
硅土矿床
siliceous earth, Dongting diwa, quartz, illite, montmorillonite