Diagenetic origin of the stratiform Cu–Co deposit at Kamoto in the Central African Copperbelt

Author:

Muchez Philippe,André-Mayer Anne-Sylvie,El Desouky Hamdy A.,Reisberg Laurie

Publisher

Springer Science and Business Media LLC

Subject

Geochemistry and Petrology,Geophysics,Economic Geology

Reference42 articles.

1. Armstrong RA, Master S, Robb LJ (2005) Geochronology of the Nchanga Granite, and constraints on the maximum age of the Katanga Supergroup, Zambian Copperbelt. J Afr Earth Sci 42:32–40

2. Barra F, Broughton D, Ruiz J, Hitzman M (2004) Multi-stage mineralization in the Zambian Copperbelt based on Re-Os isotope constraints. Geol Soc Am Abstr Programs 36:516

3. Bartholomé P, Evrard P, Katekesha F, Lopez-Ruiz J, Ngongo M (1972) Diagenetic ore-forming processes at Kamoto, Katanga, Republic of the Congo. In: Amstutz GC, Bernard AJ (eds) Ores in sediments. Springer, Heidelberg, pp 21–41

4. Batumike MJ, Cailteux JLH, Kampunzu AB (2007) Lithostratigraphy, basin development and regional correlations of the Neoproterozoic Nguba and Kundelungu rock successions, Central African Copperbelt. Gondwana Res 11:432–447

5. Bernau R, Roberts S, Richards M, Nisbet B, Boyce A, Nowecki J (2013) The geology and geochemistry of the Lumwana Cu (± Co ± U) deposits, NW Zambia. Miner Deposita 48:137–153

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