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Autor:
Sergey G. Skublov, Ekaterina V. Levashova, Maria E. Mamykina, Nikolay I. Gusev, Anatoliy I. Gusev
Publikováno v:
Записки Горного института, Vol 268, Pp 552-575 (2024)
Based on the isotopic-geochemical analyses of zircons from granites of the Belokurikhinsky massif in the Gorny Altai using the U-Pb method, the ages of three intrusion phases have been determined for the first time: the age of the first phase refers
Externí odkaz:
https://doaj.org/article/22fd1ea2f21f4d58b9a48d64459314e8
