Young silicic rocks of the Greater Caucasus
Abstract:
Rhyolites and granites of the Pliocene-Pleistocene age exposed in the collision zone of the Greater Caucasus, Russia. Includes ignimbrites and lavas associated with the Chegem caldera (2.9 Ma) and Elbrus volcano (1.98, 0.7 Ma and youger) and rhyolitic necks and granites in Tyrnyauz (1.98 Ma).
How to cite this dataset:
Shcherbakov, V., Bindeman, I., Gazeev, V., 2024. Young silicic rocks of the Greater Caucasus, Version 1.0. Interdisciplinary Earth Data Alliance (IEDA).
https://doi.org/10.60520/IEDA/113124. Accessed 2024-07-26.
DOI Creation Date:
2024-02-06
Related
Publication(s):
Shcherbakov, V., Bindeman, I., & Gazeev, V. (2022). Geochemical, Isotopic and Petrological Constraints on the Origin and Evolution of the Recent Silicic Magmatism of the Greater Caucasus. Minerals, 12(1), Article 1.
License:
Creative Commons Attribution-ShareAlike 4.0 International [CC-BY-SA-4.0]
Funding source(s):
RSF 19-17-00241
Keyword(s):
Coverage Scope: Other
Geographic Location: Greater Caucasus
User Contributed Keyword(s):
Elbrus, Chelem caldera, Tyrnyauz granite, rhyolite, ignimbrite, dacite
Data Available On:
2024-02-07