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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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.

作者简介

N. 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
俄罗斯联邦, Moscow, 119017; Moscow, 119991; Sydney; Moscow

E. Belousova

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

Email: t.romanyuk@mail.ru
澳大利亚, Sydney

M. Krupenin

Zavaritskii Institute of Geology and Geochemistry, Ural Branch

Email: t.romanyuk@mail.ru
俄罗斯联邦, Yekaterinburg, 620016

T. 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

编辑信件的主要联系方式.
Email: t.romanyuk@mail.ru
俄罗斯联邦, Moscow, 119991; Sydney; Moscow

A. Maslov

Zavaritskii Institute of Geology and Geochemistry, Ural Branch

Email: t.romanyuk@mail.ru
俄罗斯联邦, Yekaterinburg, 620016


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