Young Silicic Magmatism of the Greater Caucasus, Russia, with implication for its delamination origin based on zircon petrochronology and thermomechanical modeling-Reference-Cited by-同舟云学术

Young Silicic Magmatism of the Greater Caucasus, Russia, with implication for its delamination origin based on zircon petrochronology and thermomechanical modeling

Published:2021-04 Issue: Volume:412 Page:107173
ISSN:0377-0273
Container-title:Journal of Volcanology and Geothermal Research
language:en
Short-container-title:Journal of Volcanology and Geothermal Research

Author:

Bindeman I.N.,Colón D.P.,Wotzlaw J.-F.,Stern R.,Chiaradia M.,Guillong M.

Funder

Russian Science Foundation

Russian Science Support Foundation

Publisher

Elsevier BV

Subject

Geochemistry and Petrology,Geophysics

Reference125 articles.

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3. Repeated rhyolite eruption from heterogeneous hot zones embedded within a cool, shallow Magma reservoir;Andersen;J. Geophys. Res. Solid Earth,2019

4. The Genesis of intermediate and silicic magmas in deep crustal hot zones;Annen;J. Petrol.,2006

5. Isotopic (Nd, Sr, δ18O) signatures of the late Miocene high Sr-Ba granitoids in the Mineral’nye Vody area, Northern Caucasus: evidence of the protolith nature;Avdeenko;Dokl. Earth Sci.,2008

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