New U–Pb isotopic data for detrital zircons from metasedimentary sequences of northwestern Taimyr


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This work presents the U–Pb (LA–ICP–MS) data of detrital zircons from metasedimentary sequences of northwestern Taimyr. An analysis of the youngest populations of detrital zircons testifies to the wide distribution of Cambrian sequences in the study area, but not Precambrian sequences as was considered earlier, and the need for a substantial revision of the stratigraphic scheme of this area. The detrital zircon age distribution shows that the Timan margin of the Baltic paleocontinent was a major provenance area of the Cambrian sediments in northern and northwestern Taimyr, as well as the coeval sediments of the Severnaya Zemlya archipelago.

作者简介

V. Ershova

Institute of Earth Sciences

编辑信件的主要联系方式.
Email: ershovavictoria@gmail.com
俄罗斯联邦, St. Petersburg, 199034

A. Prokopiev

Diamond and Precious Metal Geology Institute, Siberian Branch

Email: ershovavictoria@gmail.com
俄罗斯联邦, Yakutsk, 677980

A. Khudoley

Institute of Earth Sciences

Email: ershovavictoria@gmail.com
俄罗斯联邦, St. Petersburg, 199034

V. Proskurnin

Karpinsky All-Russia Research Geological Institute

Email: ershovavictoria@gmail.com
俄罗斯联邦, St. Petersburg, 199106

T. Andersen

University of Oslo, Blindern

Email: ershovavictoria@gmail.com
挪威, Oslo, N-0316

K. Kullerud

University of Tromsø

Email: ershovavictoria@gmail.com
挪威, Tromsø, N-9037

M. Stepunina

Karpinsky All-Russia Research Geological Institute

Email: ershovavictoria@gmail.com
俄罗斯联邦, St. Petersburg, 199106

D. Kolchanov

Institute of Earth Sciences

Email: ershovavictoria@gmail.com
俄罗斯联邦, St. Petersburg, 199034

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