Email this article 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)
- Authors: Kuznetsov N.B.1,2, Romanyuk T.V.2,3, Belousova E.A.4
-
Affiliations:
- 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
- Issue: Vol 479, No 1 (2018)
- Pages: 305-309
- Section: Geology
- URL: https://ogarev-online.ru/1028-334X/article/view/192407
- DOI: https://doi.org/10.1134/S1028334X18030194
- ID: 192407
Cite item
Open Access
Access granted
Subscription Access
Abstract
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.
About the authors
N. B. Kuznetsov
Geological Institute; Gubkin Russian State University of Oil and Gas
Author for correspondence.
Email: kouznikbor@mail.ru
Russian Federation, Moscow, 119017; Moscow, 119991
T. V. Romanyuk
Gubkin Russian State University of Oil and Gas; Schmidt Institute of Physics of the Earth
Email: kouznikbor@mail.ru
Russian Federation, Moscow, 119991; Moscow
E. A. Belousova
Australian Research Council Centre of Excellence for Core to Crust Fluid Systems (CCFS)/GEMOC
Email: kouznikbor@mail.ru
Australia, Sydney
Supplementary files
