Intermediate chromitite in Kızıldağ ophiolite (SE Turkey) formed during subduction initiation in Neo-Tethys
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DOI: 10.1016/j.oregeorev.2018.10.004
Abstract: Abstract Chromitites in the Kizildag ophiolite mostly occur in the mantle harzburgites and some of them in crustal cumulate dunites. Olivine in both the dunites and chromitites is highly magnesian (Fo = 90.5–92.8 and 90.2–96.1, respectively), while… read more here.
Keywords: intermediate chromitite; olivine dunites; dunites chromitites; subduction initiation ... See more keywords