U-Pb zircon geochronology of intrusive rocks from an exotic block in the Late Cretaceous - Paleocene Tarakli Flysch (northern Turkey): Constraints on the tectonics of the Intrapontide suture zone

Di Rosa M., Farina F., Marroni M., Pandolfi L., GÖNCÜOĞLU M. C., Ellero A., ...Daha Fazla

JOURNAL OF ASIAN EARTH SCIENCES, cilt.171, ss.277-288, 2019 (SCI-Expanded) identifier identifier

  • Yayın Türü: Makale / Tam Makale
  • Cilt numarası: 171
  • Basım Tarihi: 2019
  • Doi Numarası: 10.1016/j.jseaes.2018.11.017
  • Dergi Adı: JOURNAL OF ASIAN EARTH SCIENCES
  • Derginin Tarandığı İndeksler: Science Citation Index Expanded (SCI-EXPANDED), Scopus
  • Sayfa Sayıları: ss.277-288
  • Anahtar Kelimeler: Permian granitoids, Slide-block, Foredeep, Intrapontide suture, Tarakh Flysch, Turkey, CENTRAL PONTIDES, NW TURKEY, SAKARYA ZONE, GEODYNAMIC EVOLUTION, DEVONIAN MAGMATISM, EASTERN PONTIDES, ACTIVE MARGIN, BOLU MASSIF, NE TURKEY, VARISCAN
  • Orta Doğu Teknik Üniversitesi Adresli: Evet

Özet

In the Boyali area (northern Anatolia), a thick succession of the Early Maastrichtian - Middle Paleocene Tarakli Flysch crops out. The Tarakh Flysch represents a foredeep sediment deposited during the final stage of collision between the Sakarya and Istanbul-Zonguldak continental margins, that developed as a consequence of the closure of the Intrapontide oceanic basin.