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)

A. V. Maslov; Yu. V. Erokhin; A. Gerdes; Yu. L. Ronkin; K. S. Ivanov

doi:10.1134/S1028334X18100136

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)

Авторлар: Maslov A.V.¹, Erokhin Y.V.¹, Gerdes A.², Ronkin Y.L.¹, Ivanov K.S.¹
Мекемелер:
1. Zavaritsky Institute of Geology and Geochemistry, Ural Branch
2. Goethe University
Шығарылым: Том 482, № 2 (2018)
Беттер: 1275-1277
Бөлім: Geology
URL: https://journals.rcsi.science/1028-334X/article/view/194144
DOI: https://doi.org/10.1134/S1028334X18100136
ID: 194144

Дәйексөз келтіру

Толық мәтін

Ашық рұқсат
Рұқсат жабық

Рұқсат берілді
Рұқсат жабық

Тек жазылушылар үшін

Аннотация
Авторлар туралы
Әдебиет тізімі
Қосымша файлдар
Статистика

Аннотация

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.