Geology and mineralization of the Cu-rich Mumbwa district, a potential IOCG-type system at the eastern margin of the Pan-African Hook batholith, Zambia

Author:

Milani Lorenzo,Lehmann JérémieORCID,Naydenov Kalin V.,Saalmann Kerstin,Nex Paul A.M.,Kinnaird Judith A.,Friedman Ira S.,Woolrych Thomas,Selley David

Funder

South African THRIP

Publisher

Elsevier BV

Subject

Earth-Surface Processes,Geology

Reference124 articles.

1. The geology of the Nansenga river area. Explanation of degree sheet 1526, NE quarter: report of the;Abell;Geol. Surv. Zambia,1970

2. The geology of the Lukomezi river area. Explanation of degree sheet 1526, NW quarter: report of the;Abell;Geol. Surv. Zambia,1976

3. Some aspects of the stratiform ore deposits of the Zambian Copperbelt and their genetic significance;Annels,1974

4. Radiogenic and stable isotope constraints on the genesis of the Eloise Cu–Au deposit, Cloncurry district, Northwest Queensland;Baker;Econ. Geol.,2001

5. Unraveling the origin of the Andean IOCG clan: a Re-Os isotopes approach;Barra;Ore Geol. Rev.,2017

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