The Miocene Kestanbol granitoid, in Ezine-Çanakkale, Turkey, is one of post-collision granitoids of western Anatolia, which have been related to the the late Cretaceous collision between the Anatolide-Tauride platform and the Pontides. Magmatism began during the early Miocene, with coeval alkaline to calc-alkaline plutonism and volcanism, controlled by the regional tectonic evolution. | Mineral and whole rock geochemistry of the Kestanbol granitoid (Ezine-Çanakkale) and its mafic microgranular enclaves in Northwestern Anatolia: Evidence of felsic and mafic magma interaction
