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 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 subbranch of Tosk Albanian and are descendants of the Albanian population of Eastern Thrace who migrated during the Population exchange between Greece and Turkey in the 1920s. They are known in Greece as Arvanites, a name applied to all groups of Albanian origin in Greece, but which primarily refers to the southern dialectological group of "Arbëreshë". The Albanian-speakers of Western Thrace and Macedonia use the common Albanian self-appellation, "Shqiptar". During the Ottoman Empire, Albanian communities