Located in the heart of the Lesser Caucasus mountains, where the Arabian and Eurasian tectonic plates collide, Armenia occupies an exceptional geological position shaped through millions of years of subduction and collision. It is a unique place on the Earth recording extensive intrusive and volcanic activity related to the long-standing continental convergence. The volcanoes of Armenia provide a rare opportunity to study the sources and processes involved in this unusual type of magmatism. More than 500 Quaternary volcanoes have been mapped in Armenia, most of them formed from single eruptive episodes. Among several large composite volcanoes, the mighty Aragats stands out as the largest volcano in Armenia and the region altogether. Volcani...
International audienceThis article summarizes the geodynamic evolution of the Caucasus mountain belt...
The occurrence of alkaline igneous rocks in collision zones is a topic of intense discussion with re...
Similar geological, petrological, geochemical and age features are found in various Armenian ophioli...
Located in the heart of the Lesser Caucasus mountains, where the Arabian and Eurasian tectonic plate...
Pleistocene to Holocene volcanic centres north of the Bitlis-Zagros suture in Turkey, Iran, Armenia ...
The post-collisional Syunik and Vardenis volcanic highlands, located in the southern Lesser Caucasus...
The Pliocene–Quaternary volcanic rocks of Armenia are a key component of the Arabia–Eurasia collisio...
The Tethyan geology of the Lesser Caucasus has a multiphase and complex history. The main lithotecto...
The post-collisional Syunik and Vardenis volcanic highlands, located in the southern Lesser Caucasus...
International audienceVariscan to Alpine magmatic activity on the North Tethys active Eurasian margi...
Alkaline igneous rocks are relatively rare in settings of tectonic convergence and little is known a...
Alkaline igneous rocks are relatively rare in settings of tectonic convergence and little is known a...
International audienceThe Amassia–Stepanavan blueschist-ophiolite complex of the Lesser Caucasus in ...
The southern margin of the Eurasian plate is a well-studied region of continental collision. The Cau...
Late Cenozoic volcanism in Eastern Anatolia extends in a broad SW - NE trending belt across the Arab...
International audienceThis article summarizes the geodynamic evolution of the Caucasus mountain belt...
The occurrence of alkaline igneous rocks in collision zones is a topic of intense discussion with re...
Similar geological, petrological, geochemical and age features are found in various Armenian ophioli...
Located in the heart of the Lesser Caucasus mountains, where the Arabian and Eurasian tectonic plate...
Pleistocene to Holocene volcanic centres north of the Bitlis-Zagros suture in Turkey, Iran, Armenia ...
The post-collisional Syunik and Vardenis volcanic highlands, located in the southern Lesser Caucasus...
The Pliocene–Quaternary volcanic rocks of Armenia are a key component of the Arabia–Eurasia collisio...
The Tethyan geology of the Lesser Caucasus has a multiphase and complex history. The main lithotecto...
The post-collisional Syunik and Vardenis volcanic highlands, located in the southern Lesser Caucasus...
International audienceVariscan to Alpine magmatic activity on the North Tethys active Eurasian margi...
Alkaline igneous rocks are relatively rare in settings of tectonic convergence and little is known a...
Alkaline igneous rocks are relatively rare in settings of tectonic convergence and little is known a...
International audienceThe Amassia–Stepanavan blueschist-ophiolite complex of the Lesser Caucasus in ...
The southern margin of the Eurasian plate is a well-studied region of continental collision. The Cau...
Late Cenozoic volcanism in Eastern Anatolia extends in a broad SW - NE trending belt across the Arab...
International audienceThis article summarizes the geodynamic evolution of the Caucasus mountain belt...
The occurrence of alkaline igneous rocks in collision zones is a topic of intense discussion with re...
Similar geological, petrological, geochemical and age features are found in various Armenian ophioli...