Mineralogy, composition and PGM of chromitites from Pefki, Pindos ophiolite complex (NW Greece): evidence for progressively elevated fAs conditions in the upper mantle sequence

The Pindos ophiolite complex, located in the northwestern part of continental Greece, hosts various chromite deposits of both metallurgical (high-Cr) and refractory (high-Al) type. The Pefki chromitites are banded and sub-concordant to the surrounding serpentinized dunites. The Cr# [Cr/(Cr + Al)] of...

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Veröffentlicht in:	Mineralogy and petrology 2011, Vol.101 (1-2), p.129-150
Hauptverfasser:	Kapsiotis, Argirios, Grammatikopoulos, Tassos A., Tsikouras, Basilios, Hatzipanagiotou, Konstantin, Zaccarini, Federica, Garuti, Giorgio
Format:	Artikel
Sprache:	eng
Schlagworte:	Chemistry Earth and Environmental Science Earth Sciences Geochemistry Inorganic Chemistry Low temperature Magnesium Mineralogy Original Paper Osmium Petrology Upper mantle
Online-Zugang:	Volltext
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