First Results of U–Pb LA–ICP–MS Isotope Dating of Detrital Zircons from Arkose Sandstone of the Biryan Subformation of Zilmerdak Formation (Upper Riphean, South Urals)


如何引用文章

全文:

开放存取 开放存取
受限制的访问 ##reader.subscriptionAccessGranted##
受限制的访问 订阅存取

详细

Detrital zircons (DZs) from arkose sandstones of the Upper Riphean Zilmerdak Formation (Southern Urals) yielded ages in the range of 3039–964 Ma. Grains with Late Karelian and Early and Middle Riphean ages compose 35, 34, and 26% of the total number of the analyzed zircons, respectively. This is similar to the age spectra of the Vendian sandstones (Asha Group), but it differs significantly from the age distribution typical of the Riphean stratotype sandstones.

作者简介

A. Maslov

Zavaritsky Institute of Geology and Geochemistry, Ural Branch

编辑信件的主要联系方式.
Email: amas2004@mail.ru
俄罗斯联邦, Yekaterinburg, 620016

Yu. Erokhin

Zavaritsky Institute of Geology and Geochemistry, Ural Branch

Email: amas2004@mail.ru
俄罗斯联邦, Yekaterinburg, 620016

A. Gerdes

Goethe University

Email: amas2004@mail.ru
德国, Frankfurt am Main

Yu. Ronkin

Zavaritsky Institute of Geology and Geochemistry, Ural Branch

Email: amas2004@mail.ru
俄罗斯联邦, Yekaterinburg, 620016

K. Ivanov

Zavaritsky Institute of Geology and Geochemistry, Ural Branch

Email: amas2004@mail.ru
俄罗斯联邦, Yekaterinburg, 620016

补充文件

附件文件
动作
1. JATS XML

版权所有 © Pleiades Publishing, Ltd., 2018