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Formation Peculiarities of the Franz Josef Land Volcanic Province, Arctic Ocean : The Melt Movement Direction Estimated from Anisotropy of Magnetic Susceptibility. / Abashev, V. V.; Vernikovsky, V. A.; Kazansky, A. Yu et al.

In: Doklady Earth Sciences, Vol. 486, No. 1, 01.05.2019, p. 481-484.

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

Harvard

Abashev, VV, Vernikovsky, VA, Kazansky, AY, Metelkin, DV, Mikhaltsov, NE & Bragin, VY 2019, 'Formation Peculiarities of the Franz Josef Land Volcanic Province, Arctic Ocean: The Melt Movement Direction Estimated from Anisotropy of Magnetic Susceptibility', Doklady Earth Sciences, vol. 486, no. 1, pp. 481-484. https://doi.org/10.1134/S1028334X19050106

APA

Abashev, V. V., Vernikovsky, V. A., Kazansky, A. Y., Metelkin, D. V., Mikhaltsov, N. E., & Bragin, V. Y. (2019). Formation Peculiarities of the Franz Josef Land Volcanic Province, Arctic Ocean: The Melt Movement Direction Estimated from Anisotropy of Magnetic Susceptibility. Doklady Earth Sciences, 486(1), 481-484. https://doi.org/10.1134/S1028334X19050106

Vancouver

Abashev VV, Vernikovsky VA, Kazansky AY, Metelkin DV, Mikhaltsov NE, Bragin VY. Formation Peculiarities of the Franz Josef Land Volcanic Province, Arctic Ocean: The Melt Movement Direction Estimated from Anisotropy of Magnetic Susceptibility. Doklady Earth Sciences. 2019 May 1;486(1):481-484. doi: 10.1134/S1028334X19050106

Author

Abashev, V. V. ; Vernikovsky, V. A. ; Kazansky, A. Yu et al. / Formation Peculiarities of the Franz Josef Land Volcanic Province, Arctic Ocean : The Melt Movement Direction Estimated from Anisotropy of Magnetic Susceptibility. In: Doklady Earth Sciences. 2019 ; Vol. 486, No. 1. pp. 481-484.

BibTeX

@article{dcf349bbc9a3410bb71ec3f4cd1ae5c9,
title = "Formation Peculiarities of the Franz Josef Land Volcanic Province, Arctic Ocean: The Melt Movement Direction Estimated from Anisotropy of Magnetic Susceptibility",
abstract = "Abstract: The work presents the first results on the anisotropy of magnetic susceptibility in Hooker Island basaltoids; this anisotropy is related to the direction of motion of the melt, the location of eruption centers, and the morphology of igneous bodies. The peculiarities of the primary magnetic fabric revealed correspond to a trap mechanism of formation of the Franz Josef Land igneous province and reflect the simultaneous effect of multiple small eruption centers. Earlier conclusions about the long-term (during the Early Jurassic–Early Cretaceous) multistage magmatism history have not been supported.",
keywords = "TECTONICS, MAGMATISM, EVOLUTION, SVALBARD, ISLANDS, MARGIN",
author = "Abashev, {V. V.} and Vernikovsky, {V. A.} and Kazansky, {A. Yu} and Metelkin, {D. V.} and Mikhaltsov, {N. E.} and Bragin, {V. Yu}",
year = "2019",
month = may,
day = "1",
doi = "10.1134/S1028334X19050106",
language = "English",
volume = "486",
pages = "481--484",
journal = "Doklady Earth Sciences",
issn = "1028-334X",
publisher = "PLEIADES PUBLISHING INC",
number = "1",

}

RIS

TY - JOUR

T1 - Formation Peculiarities of the Franz Josef Land Volcanic Province, Arctic Ocean

T2 - The Melt Movement Direction Estimated from Anisotropy of Magnetic Susceptibility

AU - Abashev, V. V.

AU - Vernikovsky, V. A.

AU - Kazansky, A. Yu

AU - Metelkin, D. V.

AU - Mikhaltsov, N. E.

AU - Bragin, V. Yu

PY - 2019/5/1

Y1 - 2019/5/1

N2 - Abstract: The work presents the first results on the anisotropy of magnetic susceptibility in Hooker Island basaltoids; this anisotropy is related to the direction of motion of the melt, the location of eruption centers, and the morphology of igneous bodies. The peculiarities of the primary magnetic fabric revealed correspond to a trap mechanism of formation of the Franz Josef Land igneous province and reflect the simultaneous effect of multiple small eruption centers. Earlier conclusions about the long-term (during the Early Jurassic–Early Cretaceous) multistage magmatism history have not been supported.

AB - Abstract: The work presents the first results on the anisotropy of magnetic susceptibility in Hooker Island basaltoids; this anisotropy is related to the direction of motion of the melt, the location of eruption centers, and the morphology of igneous bodies. The peculiarities of the primary magnetic fabric revealed correspond to a trap mechanism of formation of the Franz Josef Land igneous province and reflect the simultaneous effect of multiple small eruption centers. Earlier conclusions about the long-term (during the Early Jurassic–Early Cretaceous) multistage magmatism history have not been supported.

KW - TECTONICS

KW - MAGMATISM

KW - EVOLUTION

KW - SVALBARD

KW - ISLANDS

KW - MARGIN

UR - http://www.scopus.com/inward/record.url?scp=85067878077&partnerID=8YFLogxK

U2 - 10.1134/S1028334X19050106

DO - 10.1134/S1028334X19050106

M3 - Article

AN - SCOPUS:85067878077

VL - 486

SP - 481

EP - 484

JO - Doklady Earth Sciences

JF - Doklady Earth Sciences

SN - 1028-334X

IS - 1

ER -

ID: 20708084