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
Madytos (Thrace) Madytos (Thrace) Madytos (or Maitos, or Madyta) (), by the modern town of Eceabat in Turkey, was an ancient Greek city and port of Thrace, located in the region of the Thracian Chersonesos. The city was a colony of the Aeolians from Lesbos who, according to the ancient authors, founded also Sestos and Alopekonessos and other cities of the Hellespont. This was part of the Greek colonization movement of the 8th and 7th centuries BC. Later more colonists came from the Greek Ionian cities of Miletus and Clazomenae. Archaeological evidence also supports Aeolian or possibly Athenian origin of colonists. Madytos