Garnet U–Pb Age of Skarns from Dashkesan Deposit (Lesser Caucasus)


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The results of the U–Pb geochronological study of garnet from scarns of the Dashkesan deposit are reported. The first “direct” estimate of the age of the skarn formation and ore genesis for this deposit (147 ± 2 Ma) is obtained. The possibility of using the U–Pb garnet system to obtain estimates of the scarns age is shown.

Sobre autores

M. Stifeeva

Institute of Precambrian Geology and Geochronology, Russian Academy of Sciences

Autor responsável pela correspondência
Email: stifeeva.maria@yandex.ru
Rússia, St. Petersburg, 199034

E. Salnikova

Institute of Precambrian Geology and Geochronology, Russian Academy of Sciences

Email: stifeeva.maria@yandex.ru
Rússia, St. Petersburg, 199034

A. Samsonov

Institute of Geology of Ore Deposits, Petrography, Mineralogy, and Geochemistry, Russian Academy of Sciences

Email: stifeeva.maria@yandex.ru
Rússia, Moscow, 119017

A. Kotov

Institute of Precambrian Geology and Geochronology, Russian Academy of Sciences

Email: stifeeva.maria@yandex.ru
Rússia, St. Petersburg, 199034

Yu. Gritsenko

Moscow State University; Fersman Mineralogical Museum, Russian Academy
of Sciences

Email: stifeeva.maria@yandex.ru
Rússia, Moscow, 119234; Moscow, 119071

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