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View article: Electrical Conductors Beneath Mt. Erciyes Imaged by Three-dimensional Modeling of Magnetotellurics Data
Electrical Conductors Beneath Mt. Erciyes Imaged by Three-dimensional Modeling of Magnetotellurics Data Open
Earlier studies propose that the volcanic activity embodying the polygenetic Mt. Erciyes in the Cappadocian Volcanic Province (CVP), Central Anatolia, Türkiye, transpired as an inevitable product of the post-collisional extension expe…
View article: Tectonic geomorphology of the Hoyran Graben (Western Anatolia, Türkiye): insights from geomorphic indices
Tectonic geomorphology of the Hoyran Graben (Western Anatolia, Türkiye): insights from geomorphic indices Open
The area between Western Anatolia and Isparta Bend comprises numerous depressions and the active faults that bound them. The Hoyran Graben is one of these depressions, located at the northernmost part of the Isparta Bend. This NE–SW-orient…
View article: First record of tempestites from Quaternary lacustrine deposits in the Ağrı Basin (Eastern Anatolia, Türkiye): palaeoclimatological and palaeogeographic implications
First record of tempestites from Quaternary lacustrine deposits in the Ağrı Basin (Eastern Anatolia, Türkiye): palaeoclimatological and palaeogeographic implications Open
Several event layers have been identified in lacustrine deposits in the AErI Basin of Anatolia (E Türkiye). Sedimentological and palaeontological data newly indicate a storm-induced origin for some of them. The sedimentary structures in th…
View article: Van Gölü’nün (Doğu Anadolu) Holosen kıyı şeridi gelişimi üzerindeki doğal ve insan kaynaklı itici güçler: Jeomorfolojik bir yaklaşım
Van Gölü’nün (Doğu Anadolu) Holosen kıyı şeridi gelişimi üzerindeki doğal ve insan kaynaklı itici güçler: Jeomorfolojik bir yaklaşım Open
Coastal areas of the lakes are quite sensitive to climatic, hydrologic, and anthropogenic changes. These areas are also an indicator that reveals the interaction between natural driving forces and anthropogenic factors. Lake Van coastal re…
View article: Late Quaternary subsidence records from the Datça graben and Cnidus ancient city (SW Turkey): sea-level changes versus tectonics
Late Quaternary subsidence records from the Datça graben and Cnidus ancient city (SW Turkey): sea-level changes versus tectonics Open
The Datça graben in southwestern Anatolia is a WNW-trending seismically active depression, with tectonic activity since Pliocene time. This tectonic activity is controlled by normal faults, which have effected ancient settlements. The Cnid…
View article: Fluid network framing the hydrothermal system beneath Mt. Erciyes, Central Turkey
Fluid network framing the hydrothermal system beneath Mt. Erciyes, Central Turkey Open
<p>Fluid contribution in a tectonic process is a crucial parameter for characterization of its products. In the geophysical point of view, illustrating the electrical resistivity structure of any tectonic system can be used to determ…
View article: Fault-controlled deep hydrothermal flow in a back-arc tectonic setting, SE Tyrrhenian Sea
Fault-controlled deep hydrothermal flow in a back-arc tectonic setting, SE Tyrrhenian Sea Open
Understanding magmatic systems and deep hydrothermal circulation beneath arc-volcanoes provides insights into deep processes associated with slab-subduction and mantle-wedge partial melting. Here we analyze hydrothermal flow below a struct…
View article: Reconstructing the sedimentary evolution of the Miocene Aksu Basin based on fan delta development (eastern Mediterranean-Turkey)
Reconstructing the sedimentary evolution of the Miocene Aksu Basin based on fan delta development (eastern Mediterranean-Turkey) Open
The Aksu Basin in southern Turkey is dominantly represented by an alluvial fan and five fan deltas (FDs) developed along the tectonically controlled margins of the basin during the Miocene. Four alternating compressional and tensional tect…
View article: New active faults on Eurasian-Arabian collision zone: Tectonic activity of Özyurt and Gülsünler faults (Eastern Anatolian Plateau, Van-Turkey).
New active faults on Eurasian-Arabian collision zone: Tectonic activity of Özyurt and Gülsünler faults (Eastern Anatolian Plateau, Van-Turkey). Open
The Eastern Anatolian Plateau emerges from the continental collision between Arabian and Eurasian plates where intense seismicity related to the ongoing convergence characterizes the southern part of the plateau. Active deformation in this…
View article: Polyphase tectonic evolution of the Aksu Basin, Isparta Angle (Southern Turkey)
Polyphase tectonic evolution of the Aksu Basin, Isparta Angle (Southern Turkey) Open
The Aksu Basin, within the Isparta Angle, is located to the north of the intersection of the Aegean and Cyprus arcs and has been evolving since the Middle Miocene. Correlation of: (1) kinematic analysis of fault planes that cut the basin f…