Standard

Paleomagnetic data on the sedimentation rate near the Mendeleev Rise (Arctic Ocean). / Piskarev, A. L.; Andreeva, I. A.; Gus'kova, E. G.

в: Oceanology, Том 53, № 5, 01.09.2013, стр. 620-629.

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

Harvard

Piskarev, AL, Andreeva, IA & Gus'kova, EG 2013, 'Paleomagnetic data on the sedimentation rate near the Mendeleev Rise (Arctic Ocean)', Oceanology, Том. 53, № 5, стр. 620-629. https://doi.org/10.1134/S0001437013040097

APA

Piskarev, A. L., Andreeva, I. A., & Gus'kova, E. G. (2013). Paleomagnetic data on the sedimentation rate near the Mendeleev Rise (Arctic Ocean). Oceanology, 53(5), 620-629. https://doi.org/10.1134/S0001437013040097

Vancouver

Piskarev AL, Andreeva IA, Gus'kova EG. Paleomagnetic data on the sedimentation rate near the Mendeleev Rise (Arctic Ocean). Oceanology. 2013 Сент. 1;53(5):620-629. https://doi.org/10.1134/S0001437013040097

Author

Piskarev, A. L. ; Andreeva, I. A. ; Gus'kova, E. G. / Paleomagnetic data on the sedimentation rate near the Mendeleev Rise (Arctic Ocean). в: Oceanology. 2013 ; Том 53, № 5. стр. 620-629.

BibTeX

@article{f923206796764cd6b215563c8eb4436c,
title = "Paleomagnetic data on the sedimentation rate near the Mendeleev Rise (Arctic Ocean)",
abstract = "Seven cores of bottom sediments were collected during the cruise of R/V Akademik Fedorov in 2000 along the latitudinal profile crossing the Mendeleev Rise near 82° N, and then studied. The length of cores varies from 240 to 334 cm. In all cores, the boundary of the changing remanent magnetization vector corresponding to the Brunhes-Matuyama boundary was established reliably. In five cores, this boundary is at a depth of 86-102 cm; in two cores, collected to the west of the Mendeleev Rise, at depth levels of 188 and 208 cm. The correlation of paleomagnetic and lithological data demonstrates that the upper boundary of a bench of speckled pelites, overlapped by a bench of variegated pelites, is confined to the Olduvai episode or horizons lying slightly below. The average sedimentation rate of sediments from the Mendeleev Rise during the last 2-2.5 Ma have not exceeded 1-1.3 mm/ka, increasing towards the shelf seas of northeast Russia.",
author = "Piskarev, {A. L.} and Andreeva, {I. A.} and Gus'kova, {E. G.}",
year = "2013",
month = sep,
day = "1",
doi = "10.1134/S0001437013040097",
language = "English",
volume = "53",
pages = "620--629",
journal = "Oceanology",
issn = "0001-4370",
publisher = "МАИК {"}Наука/Интерпериодика{"}",
number = "5",

}

RIS

TY - JOUR

T1 - Paleomagnetic data on the sedimentation rate near the Mendeleev Rise (Arctic Ocean)

AU - Piskarev, A. L.

AU - Andreeva, I. A.

AU - Gus'kova, E. G.

PY - 2013/9/1

Y1 - 2013/9/1

N2 - Seven cores of bottom sediments were collected during the cruise of R/V Akademik Fedorov in 2000 along the latitudinal profile crossing the Mendeleev Rise near 82° N, and then studied. The length of cores varies from 240 to 334 cm. In all cores, the boundary of the changing remanent magnetization vector corresponding to the Brunhes-Matuyama boundary was established reliably. In five cores, this boundary is at a depth of 86-102 cm; in two cores, collected to the west of the Mendeleev Rise, at depth levels of 188 and 208 cm. The correlation of paleomagnetic and lithological data demonstrates that the upper boundary of a bench of speckled pelites, overlapped by a bench of variegated pelites, is confined to the Olduvai episode or horizons lying slightly below. The average sedimentation rate of sediments from the Mendeleev Rise during the last 2-2.5 Ma have not exceeded 1-1.3 mm/ka, increasing towards the shelf seas of northeast Russia.

AB - Seven cores of bottom sediments were collected during the cruise of R/V Akademik Fedorov in 2000 along the latitudinal profile crossing the Mendeleev Rise near 82° N, and then studied. The length of cores varies from 240 to 334 cm. In all cores, the boundary of the changing remanent magnetization vector corresponding to the Brunhes-Matuyama boundary was established reliably. In five cores, this boundary is at a depth of 86-102 cm; in two cores, collected to the west of the Mendeleev Rise, at depth levels of 188 and 208 cm. The correlation of paleomagnetic and lithological data demonstrates that the upper boundary of a bench of speckled pelites, overlapped by a bench of variegated pelites, is confined to the Olduvai episode or horizons lying slightly below. The average sedimentation rate of sediments from the Mendeleev Rise during the last 2-2.5 Ma have not exceeded 1-1.3 mm/ka, increasing towards the shelf seas of northeast Russia.

UR - http://www.scopus.com/inward/record.url?scp=84886558389&partnerID=8YFLogxK

U2 - 10.1134/S0001437013040097

DO - 10.1134/S0001437013040097

M3 - Article

AN - SCOPUS:84886558389

VL - 53

SP - 620

EP - 629

JO - Oceanology

JF - Oceanology

SN - 0001-4370

IS - 5

ER -

ID: 36843650