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
Western Thrace Region of Thrace boasts quite a few beautiful beaches. Additionally, there is the potential for winter tourism activities in the Rhodopi mountains, the natural border with Bulgaria which are covered by dense forest. The Muslim minority of Thrace are Greek citizens of diverse ethnic origins and is recognised as religious minority in accordance with the Treaty of Lausanne which Greece has signed with Turkey, and along with the Greek Constitution, enshrines the fundamental rights of the Turks and other ethnic groups of Eastern Macedonia and Thrace and the obligations towards them. The Greek government is not referring to the Muslim