Understanding the dynamic evolution of orogenic belts and intra-continental basins depend on field-based (tectono-) stratigraphic observations paired with geochronologic data such as Ar-40/Ar-39 analyses. Independent dating of tectono-stratigraphic units is a crucial tool to place them in a broader framework. In this study, we focus on the geodynamic development of western Anatolia, with an emphasis on the timing and progression of volcanism along the Izmir-Balikesir Transfer Zone (IBM. We present 36 new Ar-40/Ar-39 ages of both volcanic complexes/domes and volcanic rocks coevally emplaced within Miocene sediments from western Anatolian extensional basins. In combination with existing ages from the literature and paleontological records fro...
Structural analyses along selected transects across the Menderes Massif and incorporation of existin...
Following an Eocene continent-arc collision, the Western Anatolia region experienced a complete cycl...
The Southeast Anatolian Orogenic belt was formed as result of the convergence between Anatolian (Eu...
Understanding the dynamic evolution of orogenic belts and intra-continental basins depend on field-b...
The NE - SW trending G?rdes basin developed in the early Miocene as indicated by palynological data ...
To investigate the tectonic and structural mechanisms that produced the spatial-temporal patterns of...
The Izmir-Balikesir transfer zone (IBTZ) is a recently recognized strike-slip dominated shear zone t...
Apatite fission-track analyses indicate that the Kazdag. Massif in northwestern Anatolia was exhumed...
Small-mammalian faunas enable the discrimination and correlation of uppermost Lower Miocene lacustri...
Western Turkey has undergone an intense deformation which has given rise to two types of basins sinc...
Cenozoic convergence between the Eurasian and African plates and concurrent slab roll-back processes...
WOS: 000342248900016Magmatism forming the Central Anatolian Volcanic Province of Cappadocia, central...
The Alacam region of NW Turkey lies within the Alpine collision zone between the Sakarya continent a...
Abstract Apatite fission-track analyses indicate that the Kazdag ̆ Massif in northwestern Anatolia w...
The Miocene volcanic rocks along the Izmir-Balikesir Transfer Zone along the western margin of the M...
Structural analyses along selected transects across the Menderes Massif and incorporation of existin...
Following an Eocene continent-arc collision, the Western Anatolia region experienced a complete cycl...
The Southeast Anatolian Orogenic belt was formed as result of the convergence between Anatolian (Eu...
Understanding the dynamic evolution of orogenic belts and intra-continental basins depend on field-b...
The NE - SW trending G?rdes basin developed in the early Miocene as indicated by palynological data ...
To investigate the tectonic and structural mechanisms that produced the spatial-temporal patterns of...
The Izmir-Balikesir transfer zone (IBTZ) is a recently recognized strike-slip dominated shear zone t...
Apatite fission-track analyses indicate that the Kazdag. Massif in northwestern Anatolia was exhumed...
Small-mammalian faunas enable the discrimination and correlation of uppermost Lower Miocene lacustri...
Western Turkey has undergone an intense deformation which has given rise to two types of basins sinc...
Cenozoic convergence between the Eurasian and African plates and concurrent slab roll-back processes...
WOS: 000342248900016Magmatism forming the Central Anatolian Volcanic Province of Cappadocia, central...
The Alacam region of NW Turkey lies within the Alpine collision zone between the Sakarya continent a...
Abstract Apatite fission-track analyses indicate that the Kazdag ̆ Massif in northwestern Anatolia w...
The Miocene volcanic rocks along the Izmir-Balikesir Transfer Zone along the western margin of the M...
Structural analyses along selected transects across the Menderes Massif and incorporation of existin...
Following an Eocene continent-arc collision, the Western Anatolia region experienced a complete cycl...
The Southeast Anatolian Orogenic belt was formed as result of the convergence between Anatolian (Eu...