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The first paleomagnetic data on dolerites from Jeannette Island (New Siberian Islands, Arctic). / Zhdanova, A. I.; Metelkin, D. V.; Vernikovsky, V. A. et al.

In: Doklady Earth Sciences, Vol. 468, No. 2, 01.06.2016, p. 580-583.

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

Harvard

Zhdanova, AI, Metelkin, DV, Vernikovsky, VA & Matushkin, NY 2016, 'The first paleomagnetic data on dolerites from Jeannette Island (New Siberian Islands, Arctic)', Doklady Earth Sciences, vol. 468, no. 2, pp. 580-583. https://doi.org/10.1134/S1028334X16060246

APA

Zhdanova, A. I., Metelkin, D. V., Vernikovsky, V. A., & Matushkin, N. Y. (2016). The first paleomagnetic data on dolerites from Jeannette Island (New Siberian Islands, Arctic). Doklady Earth Sciences, 468(2), 580-583. https://doi.org/10.1134/S1028334X16060246

Vancouver

Zhdanova AI, Metelkin DV, Vernikovsky VA, Matushkin NY. The first paleomagnetic data on dolerites from Jeannette Island (New Siberian Islands, Arctic). Doklady Earth Sciences. 2016 Jun 1;468(2):580-583. doi: 10.1134/S1028334X16060246

Author

Zhdanova, A. I. ; Metelkin, D. V. ; Vernikovsky, V. A. et al. / The first paleomagnetic data on dolerites from Jeannette Island (New Siberian Islands, Arctic). In: Doklady Earth Sciences. 2016 ; Vol. 468, No. 2. pp. 580-583.

BibTeX

@article{791fde949050494994431c692f31f6a6,
title = "The first paleomagnetic data on dolerites from Jeannette Island (New Siberian Islands, Arctic)",
abstract = "The first paleomagnetic data on dolerite dikes from the volcanogenic–sedimentary section of Jeannette Island (De Long Archipelago, New Siberian Islands) are discussed. The petromagnetic data and results of the baked contact and fold tests are used to substantiate the nature of the characteristic magnetization component, which in combination with the 40Ar/39Ar dates implies its likely Late Precambrian–Early Paleozoic age. The calculated paleomagnetic pole makes it possible to extend the trajectory of the apparent polar movement for the New Siberian Islands block and confirms the assumption that this structural element of the Arctic shelf evolved as a terrane. Two variants of paleotectonic interpretation of the obtained data and their consistency with the available data on the geology and tectonics of the New Siberian Islands are considered.",
author = "Zhdanova, {A. I.} and Metelkin, {D. V.} and Vernikovsky, {V. A.} and Matushkin, {N. Yu}",
year = "2016",
month = jun,
day = "1",
doi = "10.1134/S1028334X16060246",
language = "English",
volume = "468",
pages = "580--583",
journal = "Doklady Earth Sciences",
issn = "1028-334X",
publisher = "PLEIADES PUBLISHING INC",
number = "2",

}

RIS

TY - JOUR

T1 - The first paleomagnetic data on dolerites from Jeannette Island (New Siberian Islands, Arctic)

AU - Zhdanova, A. I.

AU - Metelkin, D. V.

AU - Vernikovsky, V. A.

AU - Matushkin, N. Yu

PY - 2016/6/1

Y1 - 2016/6/1

N2 - The first paleomagnetic data on dolerite dikes from the volcanogenic–sedimentary section of Jeannette Island (De Long Archipelago, New Siberian Islands) are discussed. The petromagnetic data and results of the baked contact and fold tests are used to substantiate the nature of the characteristic magnetization component, which in combination with the 40Ar/39Ar dates implies its likely Late Precambrian–Early Paleozoic age. The calculated paleomagnetic pole makes it possible to extend the trajectory of the apparent polar movement for the New Siberian Islands block and confirms the assumption that this structural element of the Arctic shelf evolved as a terrane. Two variants of paleotectonic interpretation of the obtained data and their consistency with the available data on the geology and tectonics of the New Siberian Islands are considered.

AB - The first paleomagnetic data on dolerite dikes from the volcanogenic–sedimentary section of Jeannette Island (De Long Archipelago, New Siberian Islands) are discussed. The petromagnetic data and results of the baked contact and fold tests are used to substantiate the nature of the characteristic magnetization component, which in combination with the 40Ar/39Ar dates implies its likely Late Precambrian–Early Paleozoic age. The calculated paleomagnetic pole makes it possible to extend the trajectory of the apparent polar movement for the New Siberian Islands block and confirms the assumption that this structural element of the Arctic shelf evolved as a terrane. Two variants of paleotectonic interpretation of the obtained data and their consistency with the available data on the geology and tectonics of the New Siberian Islands are considered.

UR - http://www.scopus.com/inward/record.url?scp=84978539347&partnerID=8YFLogxK

U2 - 10.1134/S1028334X16060246

DO - 10.1134/S1028334X16060246

M3 - Article

AN - SCOPUS:84978539347

VL - 468

SP - 580

EP - 583

JO - Doklady Earth Sciences

JF - Doklady Earth Sciences

SN - 1028-334X

IS - 2

ER -

ID: 25469470