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
Turks of Western Thrace multiethnic character of the Muslim minority of Greece, which includes Turks, Pomaks and Roma Muslims, the Government of Greece does not refer to it by a specific ethnic background, nor does recognize any of these ethnicities, including the Turks, as separate ethnic minority in Western Thrace, instead referring to the whole Muslim minority on religious grounds, as the "Muslim Minority of Western Thrace" or "Greek Muslims". This is in accordance with the Treaty of Lausanne to which Greece, along with Turkey, is a signature member. The Lausanne Treaty, along with the Greek Constitution and the Charter of Fundamental Rights of