Undu

斐济· Cakaudrove, Vanua Levu Island未知
铜金属总量
—
平均品位
2.52%
矿床类型
VMS 双峰-酸性型
发现年份
1957

概述

Massive pods and lenses, irregular pipe-like dissemination, plunges ESE at 20?-30?, represents an exhalative center. Surface gossan 750 x 50 m, underlain by thin zone of supergene ore. Possible eruptive center 500 m to the south of deposit. Island arc tholeiites.

地质背景

构造环境: Siliciclastic-felsic in mature epicontinental arc

资源与开采

投产年份: 1968

数据溯源

数据来源: USGS MRDS