A Ismail-Zadeh, S Adamia, A Chabukiani… - Earth-Science …, 2020 - Elsevier
Being a part of ongoing continental collision between the Arabian and Eurasian plates, the Caucasus region is a remarkable site of moderate to strong seismicity, where devastating …
Abstract The Turkish–Iranian Plateau grew after the Middle Miocene following the initial Paleogene Arabia–Eurasia collision. Authors attribute uplift to break-off of the southern Neo …
Although many different mechanisms for subduction initiation have been proposed, only few of them are viable in terms of consistency with observations and reproducibility in numerical …
AM Forte, E Cowgill, KX Whipple - Tectonics, 2014 - Wiley Online Library
Abstract The Greater Caucasus Mountains, due to their youth (~ 5 Ma), provide an opportunity for insight into the early stages of orogen development during continent …
Abstract The Pliocene–Quaternary volcanic rocks of Armenia are a key component of the Arabia–Eurasia collision, representing intense magmatism within the Turkish–Iranian …
Here, we investigated the crustal structure beneath eastern Anatolia, an area of high seismicity and critical significance for earthquake hazards in Turkey. The study was based …
Stratigraphic evidence is used to interpret that the East Anatolian Plateau with 2 km average elevation today was below sea level~ 20 Ma and uplift began in the northern part. The …
T Mumladze, AM Forte, ES Cowgill, CC Trexler… - GeoResJ, 2015 - Elsevier
Abstract The Greater Caucasus Mountains contain the highest peaks in Europe and define, for over 850 km along strike, the leading edge of the second-largest active collisional orogen …