The Black Sea basins structure and history: New model based on new deep penetration regional seismic data. Part 2: Tectonic history and paleogeography
A new lithostratigraphy scheme has been compiled for the Western Black Sea Basin and a
new geological history scheme from Middle Jurassic till Neogene is suggested for the entire …
new geological history scheme from Middle Jurassic till Neogene is suggested for the entire …
Early Cretaceous sedimentation and orogeny on the active margin of Eurasia: Southern Central Pontides, Turkey
AI Okay, G Sunal, S Sherlock, D Alt ner… - …, 2013 - Wiley Online Library
Abstract The Pontides in northern Turkey constituted part of the southern active margin of
Eurasia during the Mesozoic. In the Early Cretaceous, a large submarine turbidite fan …
Eurasia during the Mesozoic. In the Early Cretaceous, a large submarine turbidite fan …
Transition from shoshonitic to adakitic magmatism in the Eastern Pontides, NE Turkey: implications for slab window melting
The formation of the eastern Pontides orogenic belt has been widely assigned to a
northward subduction of the Neotethyan oceanic slab during the late Mesozoic–Cenozoic …
northward subduction of the Neotethyan oceanic slab during the late Mesozoic–Cenozoic …
Reconciling the geological history of western Turkey with plate circuits and mantle tomography
We place the geological history since Cretaceous times in western Turkey in a context of
convergence, subduction, collision and slab break-off. To this end, we compare the west …
convergence, subduction, collision and slab break-off. To this end, we compare the west …
Mesozoic to recent geological history of southern Crimea and the Eastern Black Sea region
AM Nikishin, M Wannier, AS Alekseev… - Geological Society …, 2017 - lyellcollection.org
We provide a synthesis of stratigraphic data to unravel the history of the geological evolution
of South Crimea in the Mesozoic and Cenozoic. The South Crimea Orogen consists of three …
of South Crimea in the Mesozoic and Cenozoic. The South Crimea Orogen consists of three …
Early–middle Jurassic intra-oceanic subduction in the İzmir-Ankara-Erzincan Ocean, northern Turkey
The İzmir-Ankara-Erzincan suture zone near Çankırı comprises an ophiolite-related rock
suite of amphibolite, pyroxene-amphibolite and epidote-amphibolite. The geochemical data …
suite of amphibolite, pyroxene-amphibolite and epidote-amphibolite. The geochemical data …
Tectonic setting of the Jurassic bimodal magmatism in the Sakarya Zone (Central and Western Pontides), Northern Turkey: a geochemical and isotopic approach
The Lower to Middle Jurassic Mudurnu formation of the Sakarya Zone (Northern Turkey)
was deposited in an extensional basin. This unit crops out along the southern Pontide range …
was deposited in an extensional basin. This unit crops out along the southern Pontide range …
[图书][B] Tectono-stratigraphy of the Çankırı Basin: late Cretaceous to early Miocene evolution of the Neotethyan suture zone in Turkey
N Kaymakci, Y Özçelik, SH White, PM Van Dijk - 2009 - lyellcollection.org
The Çankırı Basin straddles the İzmir–Ankara–Erzincan Suture Zone which demarcates the
former position of the northern branch of the Neotethys. It includes more than 3 km of pre …
former position of the northern branch of the Neotethys. It includes more than 3 km of pre …
Discovery of Miocene adakitic dacite from the Eastern Pontides Belt (NE Turkey) and a revised geodynamic model for the late Cenozoic evolution of the Eastern …
The Cenozoic magmatic record within the ca. 500km long eastern Pontides orogen, located
within the Alpine metallogenic belt, is critical to evaluate the tectonic history and geodynamic …
within the Alpine metallogenic belt, is critical to evaluate the tectonic history and geodynamic …
Late Cretaceous to Paleocene oroclinal bending in the central Pontides (Turkey)
The Turkish Pontide fold‐and‐thrust belt formed since the Paleozoic and is an important
element in the Africa‐Eurasia convergence and the resulting closure of the Neo‐Tethys …
element in the Africa‐Eurasia convergence and the resulting closure of the Neo‐Tethys …