Tectonically induced Quaternary drainage diversion in the northeastern Aegean

Okay N., Okay A.

JOURNAL OF THE GEOLOGICAL SOCIETY, cilt.159, ss.393-399, 2002 (SCI-Expanded) identifier identifier

  • Yayın Türü: Makale / Tam Makale
  • Cilt numarası: 159
  • Basım Tarihi: 2002
  • Doi Numarası: 10.1144/0016-764901-065
  • Dergi Adı: JOURNAL OF THE GEOLOGICAL SOCIETY
  • Derginin Tarandığı İndeksler: Science Citation Index Expanded (SCI-EXPANDED), Scopus
  • Sayfa Sayıları: ss.393-399
  • Anahtar Kelimeler: Aegean, Balkans, North Anatolian Fault, drainage patterns, tectonics, NORTH ANATOLIAN FAULT, ACTIVE FAULTS, MARMARA SEA, TURKEY, EVOLUTION, BASIN, DEFORMATION, REGION, GREECE, THRACE
  • İstanbul Teknik Üniversitesi Adresli: Evet

Özet

The Maritsa River in the Balkans, over 500 km long, flows at present into the northern Aegean Sea. Geological and geomorphological data indicate that it was flowing into the Marmara Sea until about 1.5 Ma, and was diverted into the Aegean Sea following coseismic uplift along the North Anatolian Fault. Seismic reflection sections in the Marmara Sea indicate the presence of up to 2.5 km thick fluviatile to limnic Upper Miocene-Quaternary sediments, probably supplied by a Palaeo-Maritsa river. The drainage diversion cut off the sediment supply, with the result that the terrigeneous sediments of the Marmara Sea were depressed to a water depth of 1150 m.