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 …

Turkey is located in one of the most seismically active regions in the world. Characterizing
seismic source zones in this region requires evaluation and integration of geological …

This paper presents an inventory of the relevant information to delineate the Tethyside
sutures and the continental blocks they stitch in Turkey and to summarise their history. A …

Abstract The Central Pontides of N Turkey represents a mobile orogenic belt of the southern
Eurasian margin that experienced several phases of exhumation associated with the …

Arslantepe, located in south-eastern Turkey, is a multi-period settlement with a rich history of
habitation dating back to at least the late 5th millennium BCE and spanning into the …

Transgressive sequences of Campanian-Maastrichtian Stages in Turkey generally begin
with medium-to coarse-grained clastics and continue with shallow marine limestones, reefal …

Sedimentary successions in the northwestern Gulf of Suez provide important clues to the
understanding of the geological evolution of NE Africa during the middle and late Eocene …

Major and trace elements and Sr—Nd isotopic data are presented for the Quaternary
alkaline volcanism NW of Ahar (NW Iran). The exposed rocks mainly consist of alkali basalts …

The East Anatolian High Plateau, part of the Alpine-Himalayan orogen, is a 200 km wide,
approximately EW trending belt surrounded by two peripheral mountains of the Anatolian …

The petrographic and geochemical analyses of 130 Late Chalcolithic 3 (LC3, 3800 bce) to
Early Bronze Age IIIB (EBAIIIB, 2000 bce) ceramics from Arslantepe and the Malatya Plain in …