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 …

Abstract The Central and Eastern Anatolian plateaus are integral parts of the world's third
largest orogenic plateau. In the past decade, geophysical surveys have provided insights …

Valid palaeotectonic and palaeogeographical reconstructions of the easternmost
Mediterranean and adjacent region involve a long-lived Tethys (Rheic, Palaeotethyan and …

Uplifted Neogene marine sediments and Quaternary fluvial terraces in the Mut Basin,
southern Turkey, reveal a detailed history of surface uplift along the southern margin of the …

Submarine channels serve as routes transporting sediments across hundreds of kilometers
from continental margins to the deepest parts of a basin's seafloor. Consequently, owing to …

A revised stratigraphic framework for the Messinian succession of Cyprus is proposed
demonstrating that the three‐stage model for the Messinian salinity crisis recently …

The abundance of the major coralline algal groups has been investigated and quantified in
the coralline-rich facies of the Miocene shallow-water carbonates of the Eratosthenes …

Abstract The Cyprus Arc system constitutes a major active plate boundary in the eastern
Mediterranean region. This structure is directly linked with the northward convergence of the …

Sr isotope records from marginal marine basins track the mixing between seawater and
local continental runoff, potentially recording the effects of sea level, tectonic, and climate …

The eastern Mediterranean region is in the embryonic stages of continent-to-continent
collision, and has a pristine Miocene–Quaternary tectonic and stratigraphic record which is …