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Submarine permafrost in the nearshore zone of the southwestern Kara Sea. / Rekant, P.V.; Cherkashev, G.; Vanstein, B.; Krinitsky, P.

In: Geo-Marine Letters, Vol. 25, No. 2-3, 01.06.2005, p. 183-189.

Research output: Contribution to journal › Article

Harvard

Rekant, PV, Cherkashev, G, Vanstein, B & Krinitsky, P 2005, 'Submarine permafrost in the nearshore zone of the southwestern Kara Sea', Geo-Marine Letters, vol. 25, no. 2-3, pp. 183-189. https://doi.org/10.1007/s00367-004-0199-5

APA

Rekant, P. V., Cherkashev, G., Vanstein, B., & Krinitsky, P. (2005). Submarine permafrost in the nearshore zone of the southwestern Kara Sea. Geo-Marine Letters, 25(2-3), 183-189. https://doi.org/10.1007/s00367-004-0199-5

Vancouver

Rekant PV, Cherkashev G, Vanstein B, Krinitsky P. Submarine permafrost in the nearshore zone of the southwestern Kara Sea. Geo-Marine Letters. 2005 Jun 1;25(2-3):183-189. https://doi.org/10.1007/s00367-004-0199-5

Author

Rekant, P.V. ; Cherkashev, G. ; Vanstein, B. ; Krinitsky, P. / Submarine permafrost in the nearshore zone of the southwestern Kara Sea. In: Geo-Marine Letters. 2005 ; Vol. 25, No. 2-3. pp. 183-189.

BibTeX

@article{b443a3dbd3644c85870d2b0c159af2e3,
title = "Submarine permafrost in the nearshore zone of the southwestern Kara Sea",
abstract = "The results of seismic studies in the shallow waters of the southwestern Kara Sea show the presence of a seismic unit that can be interpreted as relict submarine permafrost. The permafrost table has a strongly dissected upper surface and is located at a water depth of 5-10 m. A 3D modeling of the permafrost table suggests the presence of relict buried thermodenudational depressions (up to 2 km across) at a water depth of 5-10 m. The depressions may be considered to be paragenetic to thermocirques found at the Shpindler site. Relict thermocirques are completely filled with sediment and not exposed at the sediment surface.",
author = "P.V. Rekant and G. Cherkashev and B. Vanstein and P. Krinitsky",
year = "2005",
month = jun,
day = "1",
doi = "10.1007/s00367-004-0199-5",
language = "English",
volume = "25",
pages = "183--189",
journal = "Geo-Marine Letters",
issn = "0276-0460",
publisher = "Springer Nature",
number = "2-3",

}

RIS

TY - JOUR

T1 - Submarine permafrost in the nearshore zone of the southwestern Kara Sea

AU - Rekant, P.V.

AU - Cherkashev, G.

AU - Vanstein, B.

AU - Krinitsky, P.

PY - 2005/6/1

Y1 - 2005/6/1

N2 - The results of seismic studies in the shallow waters of the southwestern Kara Sea show the presence of a seismic unit that can be interpreted as relict submarine permafrost. The permafrost table has a strongly dissected upper surface and is located at a water depth of 5-10 m. A 3D modeling of the permafrost table suggests the presence of relict buried thermodenudational depressions (up to 2 km across) at a water depth of 5-10 m. The depressions may be considered to be paragenetic to thermocirques found at the Shpindler site. Relict thermocirques are completely filled with sediment and not exposed at the sediment surface.

AB - The results of seismic studies in the shallow waters of the southwestern Kara Sea show the presence of a seismic unit that can be interpreted as relict submarine permafrost. The permafrost table has a strongly dissected upper surface and is located at a water depth of 5-10 m. A 3D modeling of the permafrost table suggests the presence of relict buried thermodenudational depressions (up to 2 km across) at a water depth of 5-10 m. The depressions may be considered to be paragenetic to thermocirques found at the Shpindler site. Relict thermocirques are completely filled with sediment and not exposed at the sediment surface.

UR - http://www.scopus.com/inward/record.url?scp=31444441620&partnerID=8YFLogxK

U2 - 10.1007/s00367-004-0199-5

DO - 10.1007/s00367-004-0199-5

M3 - Article

AN - SCOPUS:31444441620

VL - 25

SP - 183

EP - 189

JO - Geo-Marine Letters

JF - Geo-Marine Letters

SN - 0276-0460

IS - 2-3

ER -

ID: 35830759