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Record #104192:

The western Barents Sea during the Cenozoic / Tore O. Vorren, G. Richardsen, Stig-Morten Knutsen, E. Henriksen.

Title: The western Barents Sea during the Cenozoic / Tore O. Vorren, G. Richardsen, Stig-Morten Knutsen, E. Henriksen.
Author(s): Vorren, Tore O.
Richardsen, G.
Knutsen, Stig-Morten.
Henriksen, E.
Date: 1990.
Publisher: Dordrecht: Kluwer Academic
In: Geological history of the polar oceans : Arctic versus Antarctic. (1990.),
Abstract: Seismic reflection data and well logs used to interpret Cenozoic sedimentary environments in south-western Barents Sea. Cenozoic erosion and sedimentation rates quantified by volumentric calculation. In Svalbard area close to 3000 m have been eroded since Oligocene. Same amount or more was eroded from Stappen High during Palaeogene and Early Neogene. In south-western areas, from Eocene to Early Oligocene, erosion occurred along margin; Loppen High and adjacent areas served as source areas. During Neogene and Pleistocene average erosion in south-western Barents Sea was about 600 m. Erosion greater in south-east than in west and north, and deeper where former glacial ice streams flowed.
Notes:

In: Geological history of the polar oceans : Arctic versus Antarctic / Ulrich Bleil, Jörn Thiede, eds.

Keywords: 551.3.051 -- Sedimentation and stratification.
551.3.053 -- Geological erosion, corrosion and disintegration.
551.461.8 -- Palaeo-oceanography.
551.77 -- Cenozoic.
551.781 -- Palaeogene.
551.782 -- Neogene.
B -- Geology and soil sciences.
(*60) -- Arctic Ocean and adjacent waters.
(*686) -- Barents Sea.
SPRI record no.: 104192

MARCXML

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035 ## ‡aSPRI-104192
040 ## ‡aUkCU-P‡beng‡eaacr
245 04 ‡aThe western Barents Sea during the Cenozoic /‡cTore O. Vorren, G. Richardsen, Stig-Morten Knutsen, E. Henriksen.
260 ## ‡aDordrecht :‡bKluwer Academic,‡c1990.
300 ## ‡ap. 95-118 :‡bdiags., tables, maps.
490 0# ‡aNATO ASI Series. Series C, Mathematical and Physical Sciences ;‡v308
500 ## ‡aIn: Geological history of the polar oceans : Arctic versus Antarctic / Ulrich Bleil, Jörn Thiede, eds.
520 3# ‡aSeismic reflection data and well logs used to interpret Cenozoic sedimentary environments in south-western Barents Sea. Cenozoic erosion and sedimentation rates quantified by volumentric calculation. In Svalbard area close to 3000 m have been eroded since Oligocene. Same amount or more was eroded from Stappen High during Palaeogene and Early Neogene. In south-western areas, from Eocene to Early Oligocene, erosion occurred along margin; Loppen High and adjacent areas served as source areas. During Neogene and Pleistocene average erosion in south-western Barents Sea was about 600 m. Erosion greater in south-east than in west and north, and deeper where former glacial ice streams flowed.
650 07 ‡a551.3.051 -- Sedimentation and stratification.‡2udc
650 07 ‡a551.3.053 -- Geological erosion, corrosion and disintegration.‡2udc
650 07 ‡a551.461.8 -- Palaeo-oceanography.‡2udc
650 07 ‡a551.77 -- Cenozoic.‡2udc
650 07 ‡a551.781 -- Palaeogene.‡2udc
650 07 ‡a551.782 -- Neogene.‡2udc
650 07 ‡aB -- Geology and soil sciences.‡2local
651 #7 ‡a(*60) -- Arctic Ocean and adjacent waters.‡2udc
651 #7 ‡a(*686) -- Barents Sea.‡2udc
700 1# ‡aVorren, Tore O.
700 1# ‡aRichardsen, G.
700 1# ‡aKnutsen, Stig-Morten.
700 1# ‡aHenriksen, E.
773 0# ‡7nnam ‡aUlrich Bleil, Jörn Thiede, eds. ‡tGeological history of the polar oceans : Arctic versus Antarctic. ‡dDordrecht : Kluwer Academic, 1990. ‡wSPRI-104236
917 ## ‡aUnenhanced record from Muscat, imported 2019
948 3# ‡a20231205