Lisbon Valley

美国· Utah未知
铜金属总量
—
平均品位
0.53%
矿床类型
沉积岩容矿层状铜矿
发现年份
—

概述

Disseminated deposits adjacent to Lisbon fault; deposits|occur as veins in faults and disseminated bodies in sandstone adjacent to|the veins. Disseminated bodies are stacked at more than one stratigraphic|level.

地质背景

容矿岩石: Arkosic sandstone (Cretaceous)

地质省: 5021

资源与开采

数据溯源

数据来源: USGS MRDS