Hüseyin Kozlu

TL;DR: The Marao region of Turkey includes the Anatolian-Arabian-African triple junction as mentioned in this paper, where the Aslantao-Iskenderun zone is expressed near the triple junction, now undergoing slow left-lateral transtension.

TL;DR: The Goksun ophiolite (northern Kahramanmaras) is located in the EW-trending nappe zone of the southeast Anatolian orogenic belt as discussed by the authors, which consists of ultramafic-mafic cumulates, isotropic gabbro, a sheeted dyke complex, plagiogranite, volcanic rocks and associated volcanosedimentary units.

TL;DR: In this article, the authors present a survey of several Palaeozoic sections in both the Taurus range and the Border Folds that documents typical glacial features including a glacial pavement and striated dropstones (Halevikdere Formation) and demonstrates the former presence of an ice sheet in southern and south-eastern Turkey.

TL;DR: In this article, the Southern Zone of the Eastern Mediterranean can be divided into two distinct zones: the Northern Zone (Carpathian-Balkan, Istanbul, Zonguldak and Main Range terranes) and the Southern Zones (Tauride-Anatolide, SE Anatolian-Arabian, and Central Iranian teranes).

TL;DR: In this paper, four major sedimentary sequences are defined according to the main transgressive events and the subsequent shelf progradations in southern Turkey (Taurus Chain or Taurides) and southeastern Turkey (Border Folds of the Arabian Plate), nearly complete Cambrian to Ordovician successions are preserved.