JOURNAL OF ASIAN EARTH SCIENCES, vol.171, pp.277-288, 2019 (Peer-Reviewed Journal)
Article / Article
JOURNAL OF ASIAN EARTH SCIENCES
Science Citation Index Expanded, Scopus
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
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.