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
Turkish minorities in the former Ottoman Empire which was part of the heritage from the Ottoman rule of Egypt. Turkish minorities in the former Ottoman Empire The Turkish minorities/communities in the former Ottoman Empire refers to ethnic Turks, who are the descendants of Ottoman-Turkish settlers from Anatolia and Eastern Thrace, living outside of the modern borders of the Republic of Turkey, and in the independent states which were formerly part of the Ottoman Empire. Thus, they are not considered part of Turkey's modern diaspora, rather, due to living for centuries in their respective regions (and for centuries under Turkish rule), they are now considered "natives" or "locals"