Khandiza

乌兹别克斯坦未知
铜金属总量
—
平均品位
0.86%
矿床类型
VMS 双峰-酸性型
发现年份
1957

概述

Concordant tabular massive sulfide bodies in pyroclastic rocks and in dolomite horizon, accompanied by dissemination. Carboniferous back-arc basin along northern margin of the Baisun Precambrian massif.

地质背景

构造环境: Bimodal-felsic in epicontinental arc

资源与开采

运营方: 0

数据溯源

数据来源: USGS MRDS