İzmir‐Ankara suture as a Triassic to cretaceous Plate Boundary—data from central Anatolia
The İzmir‐Ankara suture represents part of the boundary between Laurasia and Gondwana
along which a wide Tethyan ocean was subducted. In northwest Turkey, it is associated with …
along which a wide Tethyan ocean was subducted. In northwest Turkey, it is associated with …
Crustal structure of the Eastern Anatolia Region (Turkey) based on seismic tomography
Here, we investigated the crustal structure beneath eastern Anatolia, an area of high
seismicity and critical significance for earthquake hazards in Turkey. The study was based …
seismicity and critical significance for earthquake hazards in Turkey. The study was based …
Neotethyan Ankara Melange, central Turkey in its Triassic-Eocene regional tectonic setting including accretionary melanges, magmatic arcs and continental units
A Harry Forbes Robertson, O Parlak… - International Geology …, 2023 - Taylor & Francis
ABSTRACT The classic Neotethyan Ankara Melange formed within the Triassic-Eocene
İzmir-Ankara-Erzincan ocean ('N Neotethys'), bordered in central Anatolia by the Kırşehir …
İzmir-Ankara-Erzincan ocean ('N Neotethys'), bordered in central Anatolia by the Kırşehir …
[HTML][HTML] Large-scale, crustal-block vertical extrusion between the Hines Creek and Denali faults coeval with slip localization on the Denali fault since ca. 45 Ma, Hayes …
Oblique convergence along strike-slip faults can lead to both distributed and localized
deformation. How focused transpressive deformation is both localized and maintained along …
deformation. How focused transpressive deformation is both localized and maintained along …
Thrace basin—An Oligocene clastic basin formed during the exhumation of the Rhodope Complex
Some orogenic sedimentary basins are difficult to assign to a particular category. An
example is the hydrocarbon‐bearing Thrace Basin in the northern Aegean. It has more than …
example is the hydrocarbon‐bearing Thrace Basin in the northern Aegean. It has more than …
Middle Devonian, late Carboniferous, and Triassic magmatic flare-ups in eastern Armorica (Sakarya Zone, Turkey) as revealed by detrital zircon U-Pb-Hf isotopic data
Abstract The Sakarya Zone of northern Turkey contains a well-preserved Early–Middle
Jurassic and Late Cretaceous submarine magmatic arc constructed over pre-Jurassic …
Jurassic and Late Cretaceous submarine magmatic arc constructed over pre-Jurassic …
Late Paleocene–Middle Eocene magmatic flare-up in western Anatolia
A 3000-km long magmatic belt of predominantly Eocene age extends from Anatolia into Iran
representing a major magmatic flare-up. We present new zircon U-Pb, Ar/Ar mica and …
representing a major magmatic flare-up. We present new zircon U-Pb, Ar/Ar mica and …
Zircon and Apatite U‐Pb Constraints on the Tectonic Affinity and Metamorphic History of the Blueschist‐Facies Ambelakia Unit, Mt. Ossa, Greece
In the Aegean region, the Cycladic Blueschist Unit (CBU) and the Ambelakia unit (Mt. Ossa,
Thessaly, Greece) represent early Cenozoic subduction‐related HP‐LT metamorphic …
Thessaly, Greece) represent early Cenozoic subduction‐related HP‐LT metamorphic …
Migration of the Palaeozoic magmatic front from Zagros to Alborz mountains with progressive closure of the Palaeo-Tethys Ocean; Insights from Zagros detrital zircon …
The northwest-southeast-trending Zagros Fold-and Thrust Belt in south Iran resulted from
the late Oligocene to the early Miocene collision of the Arabian and Central Iran blocks. The …
the late Oligocene to the early Miocene collision of the Arabian and Central Iran blocks. The …
Preparing the ground for plateau growth: Late Neogene Central Anatolian uplift in the context of orogenic and geodynamic evolution since the Cretaceous
Abstract Central Anatolia (Turkey) is a small and nascent example of a high orogenic
plateau, providing a natural laboratory to study processes driving plateau rise. The 1-km …
plateau, providing a natural laboratory to study processes driving plateau rise. The 1-km …