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A comparison of the evolution of diamondiferous quartz-rich rocks from the Saxonian Erzgebirge and the Kokchetav Massif: are so-called diamondiferous gneisses magmatic rocks?

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Keywords: Kokchetav Massif; P-T evolution; Saxonian Erzgebirge; SiO2-rich melt; anatexis; biotite; garnet; metasedimentary rock; muscovite; ultrahigh pressure

Document Type: Research Article

DOI: http://dx.doi.org/10.1016/S0012-821X(03)00512-0

Affiliations: Institut fur Mineralogie und Kristallchemie, Universitat Stuttgart, Azenbergstrasze 18, 70174 , Stuttgart, Germany

Publication date: November 30, 2003

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