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 and broke tombstones. There were also attacks against mosques, Turkish associations and Turkish consulates, attackers used methods like throwing stones, molotov bombs and damaging buildings. Between 300,000 and 400,000 Turks have left Western Thrace since 1923; most of them immigrated to Turkey. Western Thrace Turks have also immigrated to Germany, the Netherlands, the United States, the United Kingdom, Australia, Austria and Italy. Thus, overall there are an estimated 1 million Turks whose roots are from Western Thrace. It is estimated that there are between 25,000 and 40,000 Western Thrace Turks living in Western Europe. There are some members of the