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

2019-03-01
Di Rosa, Maria
Farina, Federico
Marroni, Michele
Pandolfi, Luca
Göncüoğlu, Mehmet Cemal
Ellero, Alessandro
Ottria, Giuseppe
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.
Citation Formats
M. Di Rosa et al., “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,” pp. 277–288, 2019, Accessed: 00, 2020. [Online]. Available: https://hdl.handle.net/11511/30073.