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Morphology of seamounts at the Mendeleev Rise, Arctic Ocean. / Gusev, Evgeny; Rekant, Pavel; Kaminsky, Valery; Krylov, Alexey; Morozov, Andrey; Shokalsky, Sergey; Kashubin, Sergey.

в: Polar Research, Том 36, № 2017, 1298901, 10.04.2017.

Результаты исследований: Научные публикации в периодических изданиях › статья › Рецензирование

Harvard

Gusev, E, Rekant, P, Kaminsky, V, Krylov, A, Morozov, A, Shokalsky, S & Kashubin, S 2017, 'Morphology of seamounts at the Mendeleev Rise, Arctic Ocean', Polar Research, Том. 36, № 2017, 1298901. https://doi.org/10.1080/17518369.2017.1298901

APA

Gusev, E., Rekant, P., Kaminsky, V., Krylov, A., Morozov, A., Shokalsky, S., & Kashubin, S. (2017). Morphology of seamounts at the Mendeleev Rise, Arctic Ocean. Polar Research, 36(2017), [1298901]. https://doi.org/10.1080/17518369.2017.1298901

Vancouver

Gusev E, Rekant P, Kaminsky V, Krylov A, Morozov A, Shokalsky S и пр. Morphology of seamounts at the Mendeleev Rise, Arctic Ocean. Polar Research. 2017 Апр. 10;36(2017). 1298901. https://doi.org/10.1080/17518369.2017.1298901

Author

Gusev, Evgeny ; Rekant, Pavel ; Kaminsky, Valery ; Krylov, Alexey ; Morozov, Andrey ; Shokalsky, Sergey ; Kashubin, Sergey. / Morphology of seamounts at the Mendeleev Rise, Arctic Ocean. в: Polar Research. 2017 ; Том 36, № 2017.

BibTeX

@article{76727ec7c9f442269f2613fab0b56c38,
title = "Morphology of seamounts at the Mendeleev Rise, Arctic Ocean",
abstract = "Geological and geophysical studies undertaken during the Russian Arktika-2012 Expedition of 2012 produced evidence of basement outcrops on the steep slopes of the Mendeleev Rise seamounts. Observations of the outcrops from research submarines showed that part of the steep slopes interpreted as basement outcrops based on seismic data were overlain by a light sediment cover. The actual areas of the basement outcrops are therefore much less than indicated by the seismic data alone. The outcrops found are of 5-10 to 100-200 m and are often stretched along some hypsometric level or arranged obliquely, crossing a slope at an angle to the horizon. The rocks are massive and layered, often strongly weathered, cavernous, with visible fissures and extended by dislocations.",
keywords = "Arctic ocean, Mendeleev ridge, Ocean geomorphology, Slope structures, Submarine landscapes",
author = "Evgeny Gusev and Pavel Rekant and Valery Kaminsky and Alexey Krylov and Andrey Morozov and Sergey Shokalsky and Sergey Kashubin",
year = "2017",
month = apr,
day = "10",
doi = "10.1080/17518369.2017.1298901",
language = "English",
volume = "36",
journal = "Polar Research",
issn = "0800-0395",
publisher = "Taylor & Francis",
number = "2017",

}

RIS

TY - JOUR

T1 - Morphology of seamounts at the Mendeleev Rise, Arctic Ocean

AU - Gusev, Evgeny

AU - Rekant, Pavel

AU - Kaminsky, Valery

AU - Krylov, Alexey

AU - Morozov, Andrey

AU - Shokalsky, Sergey

AU - Kashubin, Sergey

PY - 2017/4/10

Y1 - 2017/4/10

N2 - Geological and geophysical studies undertaken during the Russian Arktika-2012 Expedition of 2012 produced evidence of basement outcrops on the steep slopes of the Mendeleev Rise seamounts. Observations of the outcrops from research submarines showed that part of the steep slopes interpreted as basement outcrops based on seismic data were overlain by a light sediment cover. The actual areas of the basement outcrops are therefore much less than indicated by the seismic data alone. The outcrops found are of 5-10 to 100-200 m and are often stretched along some hypsometric level or arranged obliquely, crossing a slope at an angle to the horizon. The rocks are massive and layered, often strongly weathered, cavernous, with visible fissures and extended by dislocations.

AB - Geological and geophysical studies undertaken during the Russian Arktika-2012 Expedition of 2012 produced evidence of basement outcrops on the steep slopes of the Mendeleev Rise seamounts. Observations of the outcrops from research submarines showed that part of the steep slopes interpreted as basement outcrops based on seismic data were overlain by a light sediment cover. The actual areas of the basement outcrops are therefore much less than indicated by the seismic data alone. The outcrops found are of 5-10 to 100-200 m and are often stretched along some hypsometric level or arranged obliquely, crossing a slope at an angle to the horizon. The rocks are massive and layered, often strongly weathered, cavernous, with visible fissures and extended by dislocations.

KW - Arctic ocean

KW - Mendeleev ridge

KW - Ocean geomorphology

KW - Slope structures

KW - Submarine landscapes

UR - http://www.scopus.com/inward/record.url?scp=85017343194&partnerID=8YFLogxK

U2 - 10.1080/17518369.2017.1298901

DO - 10.1080/17518369.2017.1298901

M3 - Article

AN - SCOPUS:85017343194

VL - 36

JO - Polar Research

JF - Polar Research

SN - 0800-0395

IS - 2017

M1 - 1298901

ER -

ID: 9854044