The podiform chromitites in the Dagküplü and Kavak mines, Eskisehir ophiolite (NW-Turkey): Genetic implications of mineralogical and geochemical data

Mantle tectonites from Eskisehir (NW-Turkey) include high-Cr chromitites with limited variation of Cr#, ranging from 65 to 82. Mg# ratios are between 54 and 72 and chromite grains contain up to 3.71 wt% Fe2O3 and 0.30 wt% TiO2. PGE contents are variable and range from 109 to 533 pbb. Chondrite-norma...

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Veröffentlicht in:	Geologica acta 2009, Vol.7 (3), p.351-362
Hauptverfasser:	Zaccarini, F, Tarkian, M, Uysal, I, Sadiklar, M.B
Format:	Artikel
Sprache:	eng
Schlagworte:	Chromite Eskisehir ophiolite group elements group minerals Platinum Platinum-group elements Platinum-group minerals Turkey
Online-Zugang:	Volltext
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