Отправить статью по E-mail The First Results of U–Pb Isotope Dating of Detrital Zircons from the Upper Mesoproterozoic Gulliksenfellet Quartzite (Southern Part of Wedel Jarlsberg Land, Southwest Spitsbergen)
- Авторы: Kuznetsov N.B.1,2, Romanyuk T.V.2,3, Belousova E.A.4
-
Учреждения:
- Geological Institute
- Gubkin Russian State University of Oil and Gas
- Schmidt Institute of Physics of the Earth
- Australian Research Council Centre of Excellence for Core to Crust Fluid Systems (CCFS)/GEMOC
- Выпуск: Том 479, № 1 (2018)
- Страницы: 305-309
- Раздел: Geology
- URL: https://ogarev-online.ru/1028-334X/article/view/192407
- DOI: https://doi.org/10.1134/S1028334X18030194
- ID: 192407
Цитировать
Открытый доступ
Доступ предоставлен
Только для подписчиков
Аннотация
The first results of U–Pb isotopic dating (LA–ICP–MS) of detrital zircons from metasedimentary rocks of the pre-Devonian basement of the SW part of western Spitsbergen (from Upper Mezoproterozoic Gulliksenfellet quartzite) showed ages ranging from 1700 ± 25 to 2948 ± 27 Ma.
Об авторах
N. Kuznetsov
Geological Institute; Gubkin Russian State University of Oil and Gas
Автор, ответственный за переписку.
Email: kouznikbor@mail.ru
Россия, Moscow, 119017; Moscow, 119991
T. Romanyuk
Gubkin Russian State University of Oil and Gas; Schmidt Institute of Physics of the Earth
Email: kouznikbor@mail.ru
Россия, Moscow, 119991; Moscow
E. Belousova
Australian Research Council Centre of Excellence for Core to Crust Fluid Systems (CCFS)/GEMOC
Email: kouznikbor@mail.ru
Австралия, Sydney
Дополнительные файлы
