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A discussion of: “Corundum,Cr-muscovite rocks at O'Briens,Zimbabwe: the conjunction of hydrothermal desilicification and LIL-element enrichment — geochemical and isotopic evidence” by Kerrich et al.
Authors:W. Schreyer
Affiliation:(1) Institut für Mineralogie, Ruhr-Universität Bochum, Postfach 102148, D-4630 Bochum-Querenburg, Federal Republic of Germany
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