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Early Paleozoic tectonics for the New Siberian Islands terrane (Eastern Arctic). / Metelkin, D. V.; Chernova, A. I.; Vernikovsky, V. A. et al.

In: Doklady Earth Sciences, Vol. 477, No. 1, 01.11.2017, p. 1277-1281.

Research output: Contribution to journal › Article › peer-review

Harvard

Metelkin, DV, Chernova, AI, Vernikovsky, VA & Matushkin, NY 2017, 'Early Paleozoic tectonics for the New Siberian Islands terrane (Eastern Arctic)', Doklady Earth Sciences, vol. 477, no. 1, pp. 1277-1281. https://doi.org/10.1134/S1028334X17110228

APA

Metelkin, D. V., Chernova, A. I., Vernikovsky, V. A., & Matushkin, N. Y. (2017). Early Paleozoic tectonics for the New Siberian Islands terrane (Eastern Arctic). Doklady Earth Sciences, 477(1), 1277-1281. https://doi.org/10.1134/S1028334X17110228

Vancouver

Metelkin DV, Chernova AI, Vernikovsky VA, Matushkin NY. Early Paleozoic tectonics for the New Siberian Islands terrane (Eastern Arctic). Doklady Earth Sciences. 2017 Nov 1;477(1):1277-1281. doi: 10.1134/S1028334X17110228

Author

Metelkin, D. V. ; Chernova, A. I. ; Vernikovsky, V. A. et al. / Early Paleozoic tectonics for the New Siberian Islands terrane (Eastern Arctic). In: Doklady Earth Sciences. 2017 ; Vol. 477, No. 1. pp. 1277-1281.

BibTeX

@article{c3e6921800944984902b18a83b9a6a96,
title = "Early Paleozoic tectonics for the New Siberian Islands terrane (Eastern Arctic)",
abstract = "The New Siberian Islands archipelago is one of the few research objects accessible for direct study on the eastern Arctic shelf. There are several models that have different interpretations of the Paleozoic tectonic history and the structural affinity of the New Siberian Islands terrane. Some infer a direct relationship with the passive continental margin of the Siberian paleocontinent. Others connect it with the marginal basins of Baltica and Laurentia, or the Chukotka-Alaska microplate. Our paleomagnetic investigation led us to create an apparent polar wander path for the early Paleozoic interval of geological history. Based on it we can conclude that the New Siberian Islands terrane could not have been a part of these continental plates. This study considers the possible tectonic scenarios of the Paleozoic history of the Earth, presents and discusses the corresponding global reconstructions describing the paleogeography and probable mutual kinematics of the terranes of the Eastern Arctic.",
author = "Metelkin, {D. V.} and Chernova, {A. I.} and Vernikovsky, {V. A.} and Matushkin, {N. Yu}",
year = "2017",
month = nov,
day = "1",
doi = "10.1134/S1028334X17110228",
language = "English",
volume = "477",
pages = "1277--1281",
journal = "Doklady Earth Sciences",
issn = "1028-334X",
publisher = "PLEIADES PUBLISHING INC",
number = "1",

}

RIS

TY - JOUR

T1 - Early Paleozoic tectonics for the New Siberian Islands terrane (Eastern Arctic)

AU - Metelkin, D. V.

AU - Chernova, A. I.

AU - Vernikovsky, V. A.

AU - Matushkin, N. Yu

PY - 2017/11/1

Y1 - 2017/11/1

N2 - The New Siberian Islands archipelago is one of the few research objects accessible for direct study on the eastern Arctic shelf. There are several models that have different interpretations of the Paleozoic tectonic history and the structural affinity of the New Siberian Islands terrane. Some infer a direct relationship with the passive continental margin of the Siberian paleocontinent. Others connect it with the marginal basins of Baltica and Laurentia, or the Chukotka-Alaska microplate. Our paleomagnetic investigation led us to create an apparent polar wander path for the early Paleozoic interval of geological history. Based on it we can conclude that the New Siberian Islands terrane could not have been a part of these continental plates. This study considers the possible tectonic scenarios of the Paleozoic history of the Earth, presents and discusses the corresponding global reconstructions describing the paleogeography and probable mutual kinematics of the terranes of the Eastern Arctic.

AB - The New Siberian Islands archipelago is one of the few research objects accessible for direct study on the eastern Arctic shelf. There are several models that have different interpretations of the Paleozoic tectonic history and the structural affinity of the New Siberian Islands terrane. Some infer a direct relationship with the passive continental margin of the Siberian paleocontinent. Others connect it with the marginal basins of Baltica and Laurentia, or the Chukotka-Alaska microplate. Our paleomagnetic investigation led us to create an apparent polar wander path for the early Paleozoic interval of geological history. Based on it we can conclude that the New Siberian Islands terrane could not have been a part of these continental plates. This study considers the possible tectonic scenarios of the Paleozoic history of the Earth, presents and discusses the corresponding global reconstructions describing the paleogeography and probable mutual kinematics of the terranes of the Eastern Arctic.

UR - http://www.scopus.com/inward/record.url?scp=85037160724&partnerID=8YFLogxK

U2 - 10.1134/S1028334X17110228

DO - 10.1134/S1028334X17110228

M3 - Article

AN - SCOPUS:85037160724

VL - 477

SP - 1277

EP - 1281

JO - Doklady Earth Sciences

JF - Doklady Earth Sciences

SN - 1028-334X

IS - 1

ER -

ID: 9067394