Hare Hakhlil
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: White kaolinitic sandstone (Lower Cretaceous)
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: White kaolinitic sandstone (Lower Cretaceous)
数据来源: USGS MRDS