Abstract:In this study, we aimed to report preliminary Cr-spinel chemistry results from the podiform chromitites of the Mehmetalan Ophiolite to shed light on their petrogenesis and tectonic settings. Mehmetalan ophiolite is ordinarily represented by peridotite (harzburgite, dunite, serpentinite), ultramaficmafic cumulates (layered-isotropic-pegmatitic gabbro, pyroxenite-dunite intercalation). The maficultramafic lithologies are locally cut by pyroxenite and isolated diabase dykes. In the chromites, lens-shaped massive,… Show more
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