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Causes of Cretaceous Remagnetization on the Southwestern Periphery of the Archipelago of the New Siberian Islands. / Chernova, A. I.; Metelkin, D. V.; Vernikovsky, V. A. et al.

In: Doklady Earth Sciences, Vol. 481, No. 1, 01.07.2018, p. 847-851.

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

Harvard

Chernova, AI, Metelkin, DV, Vernikovsky, VA & Matushkin, NY 2018, 'Causes of Cretaceous Remagnetization on the Southwestern Periphery of the Archipelago of the New Siberian Islands', Doklady Earth Sciences, vol. 481, no. 1, pp. 847-851. https://doi.org/10.1134/S1028334X18070036

APA

Chernova, A. I., Metelkin, D. V., Vernikovsky, V. A., & Matushkin, N. Y. (2018). Causes of Cretaceous Remagnetization on the Southwestern Periphery of the Archipelago of the New Siberian Islands. Doklady Earth Sciences, 481(1), 847-851. https://doi.org/10.1134/S1028334X18070036

Vancouver

Chernova AI, Metelkin DV, Vernikovsky VA, Matushkin NY. Causes of Cretaceous Remagnetization on the Southwestern Periphery of the Archipelago of the New Siberian Islands. Doklady Earth Sciences. 2018 Jul 1;481(1):847-851. doi: 10.1134/S1028334X18070036

Author

Chernova, A. I. ; Metelkin, D. V. ; Vernikovsky, V. A. et al. / Causes of Cretaceous Remagnetization on the Southwestern Periphery of the Archipelago of the New Siberian Islands. In: Doklady Earth Sciences. 2018 ; Vol. 481, No. 1. pp. 847-851.

BibTeX

@article{4fb284b4408b4e31a7f2a7fb1ebfef74,
title = "Causes of Cretaceous Remagnetization on the Southwestern Periphery of the Archipelago of the New Siberian Islands",
abstract = "This study demonstrates rock-magnetic and paleomagnetic investigations of Devonian and Mesozoic deposits of Kotelny, Stolbovoy, and Great Lyakhovsky islands. The results indicate that local remagnetization took place on the southwestern periphery on the archipelago of the New Siberian Islands. A comparison of new data with the apparent polar wander path for Siberia shows that the remagnetization happened during collisional events between 140 and 80 Ma and affected only the marginal part of the terrane of the New Siberian Islands that was directly facing the deformation front. The consistent younging of the remagnetization age from the south to the north indicates dextral rotation of the terrane of the New Siberian Islands during its collision with Siberia.",
author = "Chernova, {A. I.} and Metelkin, {D. V.} and Vernikovsky, {V. A.} and Matushkin, {N. Yu}",
year = "2018",
month = jul,
day = "1",
doi = "10.1134/S1028334X18070036",
language = "English",
volume = "481",
pages = "847--851",
journal = "Doklady Earth Sciences",
issn = "1028-334X",
publisher = "PLEIADES PUBLISHING INC",
number = "1",

}

RIS

TY - JOUR

T1 - Causes of Cretaceous Remagnetization on the Southwestern Periphery of the Archipelago of the New Siberian Islands

AU - Chernova, A. I.

AU - Metelkin, D. V.

AU - Vernikovsky, V. A.

AU - Matushkin, N. Yu

PY - 2018/7/1

Y1 - 2018/7/1

N2 - This study demonstrates rock-magnetic and paleomagnetic investigations of Devonian and Mesozoic deposits of Kotelny, Stolbovoy, and Great Lyakhovsky islands. The results indicate that local remagnetization took place on the southwestern periphery on the archipelago of the New Siberian Islands. A comparison of new data with the apparent polar wander path for Siberia shows that the remagnetization happened during collisional events between 140 and 80 Ma and affected only the marginal part of the terrane of the New Siberian Islands that was directly facing the deformation front. The consistent younging of the remagnetization age from the south to the north indicates dextral rotation of the terrane of the New Siberian Islands during its collision with Siberia.

AB - This study demonstrates rock-magnetic and paleomagnetic investigations of Devonian and Mesozoic deposits of Kotelny, Stolbovoy, and Great Lyakhovsky islands. The results indicate that local remagnetization took place on the southwestern periphery on the archipelago of the New Siberian Islands. A comparison of new data with the apparent polar wander path for Siberia shows that the remagnetization happened during collisional events between 140 and 80 Ma and affected only the marginal part of the terrane of the New Siberian Islands that was directly facing the deformation front. The consistent younging of the remagnetization age from the south to the north indicates dextral rotation of the terrane of the New Siberian Islands during its collision with Siberia.

UR - http://www.scopus.com/inward/record.url?scp=85051193401&partnerID=8YFLogxK

U2 - 10.1134/S1028334X18070036

DO - 10.1134/S1028334X18070036

M3 - Article

AN - SCOPUS:85051193401

VL - 481

SP - 847

EP - 851

JO - Doklady Earth Sciences

JF - Doklady Earth Sciences

SN - 1028-334X

IS - 1

ER -

ID: 16075837