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: an international earth science journal |
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| Hauptverfasser: | , , , , , |
| Format: | Artigo |
| Sprache: | Inglês |
| Veröffentlicht: |
Universitat de Barcelona
2009
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| Schlagworte: | |
| Online-Zugang: | https://www.redalyc.org/articulo.oa?id=50513114004 |
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