The results of geochronological and isotope–geochemical study of zircons from tuff of the Sylvitsa Group (western slope of the Middle Urals): The origin of ash layers in Vendian rocks of the East European Platform


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Abstract

New LA-ICP-MS data on the U–Pb isotope age, Hf isotope characteristics, and concentrations of trace elements in zircons from volcanic tuff of the Upper Vendian Sylvitsa Group on the western slope of the Middle Urals are reported.

About the authors

N. B. Kuznetsov

Geological Institute; Gubkin Russian State University of Oil and Gas; Australian Research Council Centre of Excellence for Core to Crust Fluid Systems, GEMOC; Schmidt Institute of Physics of the Earth

Email: t.romanyuk@mail.ru
Russian Federation, Moscow, 119017; Moscow, 119991; Sydney; Moscow

E. A. Belousova

Australian Research Council Centre of Excellence for Core to Crust Fluid Systems, GEMOC

Email: t.romanyuk@mail.ru
Australia, Sydney

M. T. Krupenin

Zavaritskii Institute of Geology and Geochemistry, Ural Branch

Email: t.romanyuk@mail.ru
Russian Federation, Yekaterinburg, 620016

T. V. Romanyuk

Gubkin Russian State University of Oil and Gas; Australian Research Council Centre of Excellence for Core to Crust Fluid Systems, GEMOC; Schmidt Institute of Physics of the Earth

Author for correspondence.
Email: t.romanyuk@mail.ru
Russian Federation, Moscow, 119991; Sydney; Moscow

A. V. Maslov

Zavaritskii Institute of Geology and Geochemistry, Ural Branch

Email: t.romanyuk@mail.ru
Russian Federation, Yekaterinburg, 620016


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