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The Orhaneli ophiolite is approximately 50 km long, 15 km wide and 1500 m thick (Fig. 1 b; Sarifakioglu et al., 2009), and mainly consists of mantle-crust transition zone comprising mostly basal ultramafic cumulates.The transition zone is dominated by chromitite interlayered dunites, followed by wehrlites, lherzolites, harzburgites and pyroxenites and …
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In this study, mainly silicate and some sulfide micro-inclusions hosted in magnesiochromites of chromitites from Orhaneli Ophiolite Complex and Harmancık Peridotites in northwestern Turkey are studied. Existence of randomly distributed anhedral (globular), selectively oriented lamellar/needle-shaped silicate micro-inclusions and …
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