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
Gold wreaths from Thrace line of the last rulers of Ancient Thracia. Most likely it is from the Odrysian Kingdom of the fifth to first century BC and experts have valued the artifact to be worth approximately USD 100,000. Gold wreaths from Thrace The gold wreaths from Thrace are jewellery wreaths found in inner Thrace, which is within present day Bulgaria. The gold wreaths were found in the mounds and tombs of aristocrats at various locations in Thrace that have been dated to a period from the latter half of the fourth century and early part third century BC. There have been only five