During the Cenozoic widespread anorogenic magmatism, unrelated to recent supra-
subduction zone modification of its mantle source, developed within the Mediterranean and …

Western Anatolia (Turkey) experienced widespread Cenozoic magmatism after the collision
between the Sakarya (SC) and Anatolide–Tauride continental blocks (ATP) in the pre …

The Upper Triassic Siah-Kuh granitoid stock is part of a series of Triassic-Cretaceous
intrusions in the Phanerozoic Sanandaj-Sirjan zone in the Zagros orogenic belt, south …

We present a compilation and comparison of geochemical data of Aegean Eocene to
Recent magmatic rocks:(1) North Anatolian Eocene magmatic rocks (NAEM),(2) Aegean to …

In Western Anatolia, early-middle Miocene post-collisional volcanism is represented by K-
rich volcanic rocks; including calc-alkaline, high-K calc-alkaline, shoshonitic and …

The western part of the Aegean region includes several Neogene basins containing volcano-
sedimentary successions. The Neogene basins, located along the northern Menderes …

The İzmir–Balıkesir transfer zone (İBTZ) is a recently recognized strike-slip dominated shear
zone that accommodates the differential deformation between the Cycladic and Menderes …

Potassium-rich volcanic rocks of the shoshonite suite are common features of postorogenic
extensional settings inboard from subduction zones. Various petrogenetic processes and …

In the Aegean area, distinct fault patterns with their associated stress regimes are evidenced
along a curved convergent plate boundary. In this article, we analyze and review late …

The Ngondo complex is a late-collisional pluton, which was emplaced around 600 Ma along
a N030° E strike-slip shear zone in the southwestern part of the Neoproterozoic Fold Belt of …