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
Pomaks in Turkey tongue. It is very hard to estimate the number of Pomaks along with the Turkified Pomaks who live in Turkey, as they have blended into the Turkish society and have been often linguistically and culturally assimilated. According to "Milliyet" and "Turkish Daily News" reports, the number of the Pomaks along with the Turkified Pomaks in the country is about 600,000. Pomaks in Turkey The Pomaks in Turkey refers to an ethnic group, who are predominantly Muslim and speak their own dialect of Bulgarian. They mostly live in Eastern Thrace, though some are also present in Anatolia. In the census of