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


Дәйексөз келтіру

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Аннотация

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.

Авторлар туралы

V. Ershova

Institute of Earth Sciences

Хат алмасуға жауапты Автор.
Email: ershovavictoria@gmail.com
Ресей, St. Petersburg, 199034

A. Prokopiev

Diamond and Precious Metal Geology Institute, Siberian Branch

Email: ershovavictoria@gmail.com
Ресей, Yakutsk, 677980

A. Khudoley

Institute of Earth Sciences

Email: ershovavictoria@gmail.com
Ресей, St. Petersburg, 199034

V. Proskurnin

Karpinsky All-Russia Research Geological Institute

Email: ershovavictoria@gmail.com
Ресей, St. Petersburg, 199106

T. Andersen

University of Oslo, Blindern

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

K. Kullerud

University of Tromsø

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

M. Stepunina

Karpinsky All-Russia Research Geological Institute

Email: ershovavictoria@gmail.com
Ресей, St. Petersburg, 199106

D. Kolchanov

Institute of Earth Sciences

Email: ershovavictoria@gmail.com
Ресей, St. Petersburg, 199034

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