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, Maria; Farina, Federico; Marroni, Michele; Pandolfi, Luca; GÖNCÜOĞLU, MEHMET; Ellero, Alessandro; Ottria, Giuseppe

doi:10.1016/j.jseaes.2018.11.017

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, Scopus)

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.