Hammaslahti

芬兰未知
铜金属总量
—
平均品位
0.70%
矿床类型
VMS 双峰-基性型
发现年份
1966

概述

4 overlapping brecciated bodies, veins and stockwork, boundaries ill-defined, 2-20 m thickness, crops out at north end, plunges to greater than 500 m depth at south end. Parallels foliation of host rock. 3.8% S. Epicontinent rift.

地质背景

构造环境: Pelite-mafic in mature oceanic backarc

资源与开采

运营方: 0

投产年份: 1973

数据溯源

数据来源: USGS MRDS