Subduction-related Late Carboniferous to Early Permian Magmatism in the Eastern Pontides, the Camlik and Casurluk plutons: Insights from geochemistry, whole-rock Sr-Nd and in situ zircon Lu-Hf isotopes, and U-Pb geochronology
The plutons formed in late Paleozoic in the Eastern Pontides. We present the first discovery of late Paleozoic plutons from the region. Lu–Hf isotopes and trace element modeling show that the plutons have mantle origin. The plutons occurred in an extensional stage of subduction setting.