First results of U/Pb isotope dating (LA-ICP-MS) of detrital zircons from sandstones of the low Cambrian Brusov formation of the Southeastern White Sea region: A constraint for the lower age limit of the beginning of the Arctida-Baltica collision

[No abstract available]

Авторы
Kuznetsov N.B. 1, 2 , Alekseev A.S. 3 , Belousova E.A. 4 , Romanyuk T.V. 5, 6 , Reimers A.N. 3
Журнал
Doklady Earth Sciences
Номер выпуска
1
Язык
Английский
Страницы
28-32
Статус
Опубликовано
Ссылка
Внешняя ссылка
DOI
10.1134/S1028334X15010195
Том
460
Год
2015
Организации
  • 1 Institute of Geology, Russian Academy of Sciences, Moscow, Russian Federation
  • 2 Russian University of Peoples’ Friendship, Moscow, Russian Federation
  • 3 Moscow State University, Moscow, Russian Federation
  • 4 GEMOC-Center, Macquarie University, Sydney, Australia
  • 5 Schmidt Joint Institute of Physics of the Earth, Russian Academy of Sciences, Moscow, Russian Federation
  • 6 Gubkin Russian State University of Oil and Gas, Moscow, Russian Federation
Ключевые слова
age determination; Cambrian; collision zone; inductively coupled plasma method; isotopic analysis; sandstone; uranium-lead dating; zircon; Arctic Ocean; White Sea
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