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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


Дәйексөз келтіру

Толық мәтін

Ашық рұқсат Ашық рұқсат
Рұқсат жабық Рұқсат берілді
Рұқсат жабық Тек жазылушылар үшін

Аннотация

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.

Авторлар туралы

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
Ресей, 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
Австралия, Sydney

M. Krupenin

Zavaritskii Institute of Geology and Geochemistry, Ural Branch

Email: t.romanyuk@mail.ru
Ресей, 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

Хат алмасуға жауапты Автор.
Email: t.romanyuk@mail.ru
Ресей, Moscow, 119991; Sydney; Moscow

A. Maslov

Zavaritskii Institute of Geology and Geochemistry, Ural Branch

Email: t.romanyuk@mail.ru
Ресей, Yekaterinburg, 620016

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