Fluid fractionation of tungsten during granite–pegmatite differentiation and the metal source of peribatholitic W quartz veins: Evidence from the Karagwe-Ankole Belt (Rwanda)-Reference-Cited by-同舟云学术

Fluid fractionation of tungsten during granite–pegmatite differentiation and the metal source of peribatholitic W quartz veins: Evidence from the Karagwe-Ankole Belt (Rwanda)

Published:2016-02 Issue: Volume:175 Page:299-318
ISSN:0016-7037
Container-title:Geochimica et Cosmochimica Acta
language:en
Short-container-title:Geochimica et Cosmochimica Acta

Author:

Hulsbosch Niels,Boiron Marie-Christine,Dewaele Stijn,Muchez Philippe

Funder

Agency for Innovation by Science and Technology

Dirk Vogel Fund

French National Research Agency

KU Leuven Special Research Fund

GMD-MINIRENA

GMC

Eurotrade International S.A.R.L.

RMCA

Publisher

Elsevier BV

Subject

Geochemistry and Petrology

Reference91 articles.

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3. Validation of LA-ICP-MS fluid inclusion analysis with synthetic fluid inclusions;Allan;Am. Mineral.,2005

4. Systematic use of trace element in igneous process;Allègre;Contrib. Mineral. Petr.,1977

5. Tin and tungsten behavior in ore-bearing acidic magmatic rocks according to analyses of the partition coefficients;Antipin;Geokhimiya,1981

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