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)

被引：14

作者：

Maslov, A. V. ^{[1
]}

Erokhin, Yu. V. ^{[1
]}

Gerdes, A. ^{[2
]}

Ronkin, Yu. L. ^{[1
]}

Ivanov, K. S. ^{[1
]}

机构：

[1] Russian Acad Sci, Zavaritsky Inst Geol & Geochem, Ural Branch, Ekaterinburg 620016, Russia

[2] Goethe Univ, Frankfurt, Germany

来源：

DOKLADY EARTH SCIENCES | 2018年 / 482卷 / 02期

基金：

俄罗斯基础研究基金会;

关键词：

DEPOSITS;

D O I：

10.1134/S1028334X18100136

中图分类号：

P [天文学、地球科学];

学科分类号：

07 ;

摘要：

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.

引用

页码：1275 / 1277

页数：3

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