Thrace Basin Thrace Basin The European side of Turkey is called the Thrace Basin. It is the largest and thickest Cenozoic sedimentary basin in Turkey. The basin is triangular shaped, trends WNW-ESE and was formed by extension in late Middle Eocene to latest Oligocene times. This gas prone basin is located northwest of Istanbul, Turkey. About 9,000 meters of Eocene-Miocene marine clastics and continental sediments were deposited. Several basement faults were reactivated and underwent strike-slip motion in late Miocene times where the famous North Anatolian Fault bounds the southern part of the basin. The Cenozoic sedimentary succession, overlying Paleozoic to Mesozoic metamorphic
Albanian-speakers of Western Thrace Muslims of Western Thrace and the Christians of Istanbul. Under this provision, the Albanian Orthodox community of Eastern Thrace, was re-accommodated in Western Thrace, where they settled mainly in new and ethnically homogeneous villages built in order to receive the refugees. Today, this population lives in the same villages, but a part emigrated to bigger towns such as Thessaloniki and Athens, making the Albanian language less used. Albanian-speakers inhabit 15 homogeneous and 14 mixed villages: Albanian-speakers of Western Thrace Albanian-speakers form a linguistic minority in Greek Macedonia and Western Thrace along the border with Turkey. They speak the Northern Tosk