The Ecemiş fault, which has a left-lateral strike-slip character, separates the Pozantı-Karsantı ophiolite and the underlying Aladağ platform consisting of extensively deformed Paleozoic-Early Mesozoic carbonate rocks (Tekeli et al., 1984) at the west of the Bolkar massif and ophiolitic rocks (Dilek and Moores, 1990).The mélange and the Aladağ platform are tectonically overlain by the ...
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