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

Turkey forms one of the most actively deforming regions in the world and has a long history
of devastating earthquakes. The belter understanding of its neotectonic features and active …

We use the GPS velocity field (1988–1998) for eastern Mediterranean and Asia Minor to
determine the crustal deformation strain rate field in an area bounded by 35° N and 43° N …

Abstract The East Anatolian Fault System (EAFS) is the second major fault system in Turkey,
following the North Anatolian Fault System (NAFS). Unlike the NAFS, which produced 11 …

Abstract The January 24, 2020 Sivrice-Elazığ (Mw= 6.8) earthquake occurred on the East
Anatolian Fault zone. Main shock of this earthquake was occurred 20: 55 at local time. The …

The Quaternary alkaline volcanism of Kula is located in a western Anatolian graben system
that resulted from an Aegean extensional regime. The typically silica-undersaturated …

The East Anatolian Fault Zone (EAFZ) is among the most important active continental
transform fault zones in the world as testified by major historical and minor instrumental …

Extensive continental collision-related volcanism occurred in Turkey during Neogene–
Quaternary times. In central Anatolia, calc-alkaline to alkaline volcanism began in the Middle …

Majority of researchers consider the Arabian-Caucasus region as a corridor for migration of
earliest hominins from their African motherland to Eurasia. The paper is devoted to …

We investigate the left-lateral slip on the 240-km-long, NE-SW-trending, Malatya-Ovacik fault
zone in eastern Turkey. This fault zone splays southwestward from the North Anatolian fault …