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Paleomagnetic Evidence for the Iceland Plume Paleogeographic Stationarity and Early Cretaceous Manifestation in the High Arctic. / Metelkin, D. V.; Abashev, V. V.; Vernikovsky, V. A. et al.

In: Doklady Earth Sciences, Vol. 501, No. 2, 3, 12.2021, p. 1015-1019.

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

Harvard

Metelkin, DV, Abashev, VV, Vernikovsky, VA & Mikhaltsov, NE 2021, 'Paleomagnetic Evidence for the Iceland Plume Paleogeographic Stationarity and Early Cretaceous Manifestation in the High Arctic', Doklady Earth Sciences, vol. 501, no. 2, 3, pp. 1015-1019. https://doi.org/10.1134/S1028334X21120072

APA

Metelkin, D. V., Abashev, V. V., Vernikovsky, V. A., & Mikhaltsov, N. E. (2021). Paleomagnetic Evidence for the Iceland Plume Paleogeographic Stationarity and Early Cretaceous Manifestation in the High Arctic. Doklady Earth Sciences, 501(2), 1015-1019. [3]. https://doi.org/10.1134/S1028334X21120072

Vancouver

Metelkin DV, Abashev VV, Vernikovsky VA, Mikhaltsov NE. Paleomagnetic Evidence for the Iceland Plume Paleogeographic Stationarity and Early Cretaceous Manifestation in the High Arctic. Doklady Earth Sciences. 2021 Dec;501(2):1015-1019. 3. doi: 10.1134/S1028334X21120072

Author

Metelkin, D. V. ; Abashev, V. V. ; Vernikovsky, V. A. et al. / Paleomagnetic Evidence for the Iceland Plume Paleogeographic Stationarity and Early Cretaceous Manifestation in the High Arctic. In: Doklady Earth Sciences. 2021 ; Vol. 501, No. 2. pp. 1015-1019.

BibTeX

@article{35cd0d7fd21c46339849bc5759c43e80,
title = "Paleomagnetic Evidence for the Iceland Plume Paleogeographic Stationarity and Early Cretaceous Manifestation in the High Arctic",
abstract = "Here we present reconstructions indicating the stationary position and paleogeography of the Iceland plume, as well as its direct connection to the Mesozoic–Cenozoic large igneous provinces of the northern Atlantic and the Arctic. The main evidence for the stationary position of the Iceland hotspot comes from paleomagnetic data for the trap formation of the Franz Josef Land archipelago. Our reconstructions show that the Barents Sea magmatic province included in these traps belongs to the trace of the Iceland plume and formed as part of the High Arctic Large Igneous Province during a single relatively brief event ca. 125 Ma. Older pulses of basaltic magmatism inferred previously for the Franz Josef Land archipelago for the Early and Middle Jurassic period do not have known analogs in adjacent territories of the present-day Arctic.",
keywords = "Early Cretaceous paleogeography of the Arctic, Franz Josef Land archipelago, High Arctic Large Igneous Province, Iceland hotspot",
author = "Metelkin, {D. V.} and Abashev, {V. V.} and Vernikovsky, {V. A.} and Mikhaltsov, {N. E.}",
note = "Funding Information: The work was carried out with the support of the RSF (projects 19-17-00091, 21-17-00052). Publisher Copyright: {\textcopyright} 2021, Pleiades Publishing, Ltd.",
year = "2021",
month = dec,
doi = "10.1134/S1028334X21120072",
language = "English",
volume = "501",
pages = "1015--1019",
journal = "Doklady Earth Sciences",
issn = "1028-334X",
publisher = "PLEIADES PUBLISHING INC",
number = "2",

}

RIS

TY - JOUR

T1 - Paleomagnetic Evidence for the Iceland Plume Paleogeographic Stationarity and Early Cretaceous Manifestation in the High Arctic

AU - Metelkin, D. V.

AU - Abashev, V. V.

AU - Vernikovsky, V. A.

AU - Mikhaltsov, N. E.

N1 - Funding Information: The work was carried out with the support of the RSF (projects 19-17-00091, 21-17-00052). Publisher Copyright: © 2021, Pleiades Publishing, Ltd.

PY - 2021/12

Y1 - 2021/12

N2 - Here we present reconstructions indicating the stationary position and paleogeography of the Iceland plume, as well as its direct connection to the Mesozoic–Cenozoic large igneous provinces of the northern Atlantic and the Arctic. The main evidence for the stationary position of the Iceland hotspot comes from paleomagnetic data for the trap formation of the Franz Josef Land archipelago. Our reconstructions show that the Barents Sea magmatic province included in these traps belongs to the trace of the Iceland plume and formed as part of the High Arctic Large Igneous Province during a single relatively brief event ca. 125 Ma. Older pulses of basaltic magmatism inferred previously for the Franz Josef Land archipelago for the Early and Middle Jurassic period do not have known analogs in adjacent territories of the present-day Arctic.

AB - Here we present reconstructions indicating the stationary position and paleogeography of the Iceland plume, as well as its direct connection to the Mesozoic–Cenozoic large igneous provinces of the northern Atlantic and the Arctic. The main evidence for the stationary position of the Iceland hotspot comes from paleomagnetic data for the trap formation of the Franz Josef Land archipelago. Our reconstructions show that the Barents Sea magmatic province included in these traps belongs to the trace of the Iceland plume and formed as part of the High Arctic Large Igneous Province during a single relatively brief event ca. 125 Ma. Older pulses of basaltic magmatism inferred previously for the Franz Josef Land archipelago for the Early and Middle Jurassic period do not have known analogs in adjacent territories of the present-day Arctic.

KW - Early Cretaceous paleogeography of the Arctic

KW - Franz Josef Land archipelago

KW - High Arctic Large Igneous Province

KW - Iceland hotspot

UR - http://www.scopus.com/inward/record.url?scp=85122077108&partnerID=8YFLogxK

UR - https://www.elibrary.ru/item.asp?id=47549970

UR - https://www.mendeley.com/catalogue/d7eae4eb-4ec1-37e4-a494-a8f1501b7994/

U2 - 10.1134/S1028334X21120072

DO - 10.1134/S1028334X21120072

M3 - Article

AN - SCOPUS:85122077108

VL - 501

SP - 1015

EP - 1019

JO - Doklady Earth Sciences

JF - Doklady Earth Sciences

SN - 1028-334X

IS - 2

M1 - 3

ER -

ID: 35174584