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.

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M. Stifeeva

Institute of Precambrian Geology and Geochronology, Russian Academy of Sciences

编辑信件的主要联系方式.
Email: stifeeva.maria@yandex.ru
俄罗斯联邦, St. Petersburg, 199034

E. Salnikova

Institute of Precambrian Geology and Geochronology, Russian Academy of Sciences

Email: stifeeva.maria@yandex.ru
俄罗斯联邦, St. Petersburg, 199034

A. Samsonov

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

Email: stifeeva.maria@yandex.ru
俄罗斯联邦, Moscow, 119017

A. Kotov

Institute of Precambrian Geology and Geochronology, Russian Academy of Sciences

Email: stifeeva.maria@yandex.ru
俄罗斯联邦, St. Petersburg, 199034

Yu. Gritsenko

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

Email: stifeeva.maria@yandex.ru
俄罗斯联邦, Moscow, 119234; Moscow, 119071

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