Transition from a singly vergent to doubly vergent wedge in a young orogen: The Greater Caucasus

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 …

Pliocene–Quaternary volcanic rocks of NW Armenia: magmatism and lithospheric dynamics within an active orogenic plateau

I Neill, K Meliksetian, MB Allen, G Navarsardyan… - Lithos, 2013 - Elsevier
Abstract The Pliocene–Quaternary volcanic rocks of Armenia are a key component of the
Arabia–Eurasia collision, representing intense magmatism within the Turkish–Iranian …

Distal tephras along the SE European margin date powerful explosive eruptions from the Elbrus volcanic center (Greater Caucasus)

V Ponomareva, M Portnyagin, M Danišík… - Quaternary Science …, 2023 - Elsevier
Abstract Knowledge of temporal patterns of past explosive eruptions is necessary to
understand possible future eruptive behavior. However, volcanic records based on …

[HTML][HTML] Subducted, detached, and torn slabs beneath the Greater Caucasus

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 …

Petrology and geochemistry of the Quaternary mafic volcanism to the NE of Lake Van, Eastern Anatolian Collision Zone, Turkey

V Oyan, M Keskin, VA Lebedev, AV Chugaev… - Journal of …, 2017 - academic.oup.com
Collision-related Quaternary mafic volcanism to the north of Lake Van (Eastern Anatolia,
Turkey) occurred by eruptions from both volcanic centres and extensional fissures trending …

[HTML][HTML] The Caucasian-Arabian segment of the Alpine-Himalayan collisional belt: Geology, volcanism and neotectonics

E Sharkov, V Lebedev, A Chugaev, L Zabarinskaya… - Geoscience …, 2015 - Elsevier
Abstract The Caucasian-Arabian belt is part of the huge late Cenozoic Alpine-Himalayan
orogenic belt formed by collision of continental plates. The belt consists of two domains: the …

Late pleistocene tendürek volcano (eastern Anatolia, Turkey). II. Geochemistry and petrogenesis of the rocks

VA Lebedev, AV Chugaev, E Ünal, EV Sharkov… - Petrology, 2016 - Springer
The series of two papers presents a comprehensive isotope-geochronological and
petrologicalgeochemical study of the Late Quaternary Tendürek Volcano (Eastern Turkey) …

Detrital orthopyroxene as a tracer of geodynamic setting:: A Raman and SEM-EDS provenance study

L Borromeo, S Andò, D Bersani, E Garzanti, P Gentile… - Chemical …, 2022 - Elsevier
Raman spectroscopy is a powerful and efficient tool that is being used more and more
frequently in high-resolution provenance analysis. This study is dedicated to Ca-poor …

[HTML][HTML] At the onset of settled pastoralism–Implications of archaeozoological and isotope analyses from Bronze age sites in the North Caucasus

S Reinhold, J Eger, N Benecke, C Knipper… - Quaternary …, 2024 - Elsevier
Bioarchaeological studies provide a valuable contribution to the understanding of the
economy and activities of prehistoric populations in mountain regions. The Late Bronze Age …

Age of the magma chamber and its physicochemical state under Elbrus Greater Caucasus, Russia using zircon petrochronology and modeling insights

IN Bindeman, OE Melnik, M Guillong, IS Utkin… - Scientific Reports, 2023 - nature.com
Abstract Mount Elbrus, Europe's tallest and largely glaciated volcano, is made of silicic lavas
and is known for Holocene eruptions, but the size and state of its magma chamber remain …