Pyhasalmi

芬兰未知
铜金属总量
0.7 Mt
平均品位
0.90%
矿床类型
VMS 双峰-酸性型
发现年份
1958

概述

Massive, banded, dissemination, lens, 0.08 km thickness. 1909 +/- 27 Ma (Pb-Pb for ore galena). Remobilization of mineralization into fractures. Disseminated ore shows breccia structure, interpreted as stringer zone. 37% S, 4.9% BaO. Calc-alkaline, mature island arc. Low K rhyolite.

地质背景

构造环境: Bimodal-felsic in epicontinental arc

资源与开采

运营方: 0

投产年份: 1962

数据溯源

数据来源: USGS MRDS