Olivine/silicate melt partitioning of germanium: an example of a nearly constant partition coefficient
Author:
Publisher
Elsevier BV
Subject
Geochemistry and Petrology
Reference20 articles.
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3. Germanium content of tektites and other natural glasses; Implications concerning the origin of tektites;Cohen,1960
4. High pressure studies of the system Mg2GeO4-Mg2SiO4, with special reference to the olivine-spinel transition;Dachille;Am. Jour. Sci.,1960
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