Israil

概述

Massive, tabular, 60 m thick, 300 m below surface, strikes N30?E, dips steeply ESE. Central solid part of orebody contains 30-40% S. Downdip, orebody splits into veins and disappears. Cut by veins of chalcopyrite, strikes N60?W.

地质背景

构造环境: Bimodal-felsic in epicontinental arc

资源与开采

数据溯源

数据来源: USGS MRDS