The basins and orogens of the Mediterranean region ultimately result from the opening of
oceans during the early break-up of Pangea since the Triassic, and their subsequent …

Edge detection methods based on derivatives of potential fields have been commonly
utilizing to interpret the potential field data. Although these techniques are very useful tools …

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 …

In many fold‐thrust belts, cross section–derived shortening estimates are significantly lower
than predicted based on plate convergence. This has led to controversial hypotheses that …

Water–rock interaction in the geothermal systems related to post-collision zone volcanism: A
case study based on multivariate statistical analysis from the Kavak geothermal field (Konya …

The junction between the Aegean and Cyprus arc in the southern Turkey forms a triangular-
shaped morphological structure so-called Isparta Angle (IA). In Neogene time, the inner part …

The modern physiography of central Turkey is dominated by the 1-km-high Central
Anatolian Plateau and the Central Tauride mountains that form the southern plateau margin …

The geology, the geophysics, and other components of the solid earth system have much to
contribute to our understanding of the Mediterranean region, from the Tethys paleo …