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Peridotite massif of Goleshi is representative of the dippiest mantle section of Vardari oceanic lithosphere: The characteristics of deep mantle peridotite are: the total lack of pyroxenite dyke series, the total lack of the gabbroic dyke series, the lack of the chromites ore bodies, presence of rare and small dunite lenses. Ophiolitic peridotite of the Goleshi massif set tectonically over metamorphic Paleozoic-Triassic series and is transgresivelly overlaid by Pliocene formations. The striking of the foliation is...