Melt-rock interaction as a factor controlling evolution of chromite...

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https://www.academia.edu/119814581/Melt_rock_interaction_as_a_factor_controlling_evolution_of_chromite_and_olivine_in_dunite_case_study_from_the_Kukes_Massif_Mirdita_ophiolite_Albania

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Melt-rock interaction as a factor controlling evolution of chromite and olivine in dunite -case study from the Kukes Massif (Mirdita ophiolite, Albania

The ultramafic Kukes Massif is located in the eastern part of the Mirdita ophiolite (N Albania), which is recognised as representing Supra-Subduction lithosphere. It comprises a thick (0.8-2.5 km) dunite zone containing abundant occurrences of

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