Hypersaline fluids generated by high-grade metamorphism of evaporites: fluid inclusion study of uranium occurrences in the Western Zambian Copperbelt

Author:

Eglinger Aurélien,Ferraina Clément,Tarantola Alexandre,André-Mayer Anne-Sylvie,Vanderhaeghe Olivier,Boiron Marie-Christine,Dubessy Jean,Richard Antonin,Brouand Marc

Publisher

Springer Science and Business Media LLC

Subject

Geochemistry and Petrology,Geophysics

Reference132 articles.

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2. Andersen T, Austrheim A, Burke EA, Elvevold S (1993) N2 and CO2 in deep crustal fluids: evidence from the Caledonides of Norway. Chem Geol 108:113–132

3. 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

4. Arthurs JW, Legg CA (1974) The Geology of the Solwezi Area: Explanation of Degree Sheets 1126, NW. Quarter, and 1126, Part of SW. Quarter. Government Printer

5. Audeoud D (1982) Les minéralisations uranifères et leur environnement à Kamoto, Kambove et Shinkolobwe (Shaba, Zaïre): pétrographie, géochimie et inclusions fluides. Dissertation, Université Claude Bernard-Lyon1, France

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