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Record #104192:
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Main publication details
MARC recordThe 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 |
LDR 02045naa#a2200000#a#4500 001 SPRI-104192 005 20231205022056.0 007 ta 008 231205s1990####ne#ab##|#####|0||#0#eng#d 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