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., ...More

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

  • Publication Type: Article / Article
  • Volume: 171
  • Publication Date: 2019
  • Doi Number: 10.1016/j.jseaes.2018.11.017
  • Journal Name: JOURNAL OF ASIAN EARTH SCIENCES
  • Journal Indexes: Science Citation Index Expanded (SCI-EXPANDED), Scopus
  • Page Numbers: pp.277-288
  • Keywords: 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
  • Middle East Technical University Affiliated: Yes

Abstract

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.