The Genesis and Controls of Gold Mineralization South of Rehoboth, Namibia
Gold mineralization is hosted within gossanous quartz-haematite veins in volcano-sedimentary lithologies of the Klein Aub - Rehoboth basin of the Irumide Belt, Namibia. Mineralization and hydrothermal alteration are restricted to deformed lithologies particularly the metasediments.
Attachment | Size |
---|---|
The Genesis and Controls of Gold Mineralization South of Rehoboth_Namibia.pdf | 20.59 MB |