Har Timna
以色列未知
概述
Mobilzation of Cu in dolomite and redeposition in sandstone beds probably occurred in Miocene.
地质背景
容矿岩石: Sandstone and shale, phosphorite, Mn-rich shale (L. Cambrian)
资源与开采
数据溯源
数据来源: USGS MRDS
Mobilzation of Cu in dolomite and redeposition in sandstone beds probably occurred in Miocene.
容矿岩石: Sandstone and shale, phosphorite, Mn-rich shale (L. Cambrian)
数据来源: USGS MRDS