The carbonate-hosted willemite prospects of the Zambezi Metamorphic Belt (Zambia)-Reference-Cited by-同舟云学术

The carbonate-hosted willemite prospects of the Zambezi Metamorphic Belt (Zambia)

Published:2011-02-08 Issue:7 Volume:46 Page:707-729
ISSN:0026-4598
Container-title:Mineralium Deposita
language:en
Short-container-title:Miner Deposita

Author:

Boni Maria,Terracciano Rosario,Balassone Giuseppina,Gleeson Sarah A.,Matthews Alexander

Publisher

Springer Science and Business Media LLC

Subject

Geochemistry and Petrology,Geophysics,Economic Geology

Link

http://link.springer.com/content/pdf/10.1007/s00126-011-0338-7.pdf

Reference85 articles.

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2. Banks DA, Boyce AJ, Samson IM (2002) Constraints on the origins of fluids forming Irish Zn–Pb–Ba deposits: evidence from the composition of fluid inclusions. Econ Geol 97:471–480

3. Batchelor CE, Kinnaird JA (1984) Gahnite compositions compared. Mineral Mag 48:425–429

4. Bhalla RJ, White EW (1972) Cathodoluminescence characteristics of Mn2+-activated willemite (Zn2SiO4) single crystals. J Electrochem Soc 119:740–743

5. Binda PL (1994) Stratigraphy of the Zambian Copperbelt orebody. J Afr Earth Sci 19:251–264

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