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The Sakarya zone in Anatolia is a continental fragment >1500 km long and 120 km wide. This continent is divided into three zones: western, central and eastern. This volcanism is related to western Anatolia orogenic belt around Sakarya zone which produced Late Eocene-Late Miocene-aged mainly acidic and intermediate volcanic rocks. They are mainly composed of andesite, dacite, and latite lavas with associated pyroclastic rocks. The central Sakarya zone volcanic unit is mainly composed of Eocene-aged andesite and dac...