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?

Author: Massonne H.-J.

Source: Earth and Planetary Science Letters, Volume 216, Number 3, 30 November 2003 , pp. 347-364(18)

Publisher: Elsevier

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

Language: English

Document Type: Research article

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

Affiliations: 1: Institut fur Mineralogie und Kristallchemie, Universitat Stuttgart, Azenbergstrasze 18, 70174 , Stuttgart, Germany

Publication date: 2003-11-30

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