Инд. авторы:	Vetrov E.V., Uvarov A.N., Vishnevskaya I.A., Chervyakovskaya M.V., Vetrova N.I., Zhimulev F.I., Andreeva E.S.
Заглавие:	Structure, age, geochemical and isotope-geochemical (SM/ND) composition of the serligskaya formation, tannu-ola terrain of tuva
Библ. ссылка:	Vetrov E.V., Uvarov A.N., Vishnevskaya I.A., Chervyakovskaya M.V., Vetrova N.I., Zhimulev F.I., Andreeva E.S. Structure, age, geochemical and isotope-geochemical (SM/ND) composition of the serligskaya formation, tannu-ola terrain of tuva // Геология и минерально-сырьевые ресурсы Сибири. - 2020. - Vol.2020. - Iss. 1. - P.81-94. - ISSN 2078-0575.
Внешние системы:	DOI: 10.20403/2078-0575-2020-1-81-94; SCOPUS: 2-s2.0-85090911263;
Реферат:	eng: The Serligskaya Formation constituting the main part of the Tannu-Ola terrain is composed of differentiated series from tholeitic basalts to plagiorhyolites, formed in the conditions of immature ocean island arc. The age of Serligskaya Formation is the Early Cambrian. The source of Serligskie magmas has mantle nature (εNd(T) from +5,7 to +7,7) and model age of 550-760 Ma (Late Riphean-Vendian). © 2020 Siberian Research Institute of Geology, Geophysics and Mineral Resources. All rights reserved.
Ключевые слова:	Zircon; Volcanism; Tuva; Tannu-Ola terrain; Isotope geochemistry; Geochronology; Cambrian;
Издано:	2020
Физ. характеристика:	с.81-94