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Record #199813:

Det västantarktiska istäckets tillbakadragande efter den senaste istidens maximala utbredning = The retreat of the West Antarctic ice sheet since the last glacial maximum / Martin Jakobsson, and 7 others.

Title: Det västantarktiska istäckets tillbakadragande efter den senaste istidens maximala utbredning = The retreat of the West Antarctic ice sheet since the last glacial maximum / Martin Jakobsson, and 7 others.
Author(s): Jakobsson, Martin.
Date: 2011.
In: Polarforskningssecretariatet Årsbok = Swedish Polar Research Secretariat Yearbook. (2011.), Vol. 2010 (2011)
Abstract: Overview of research during 2009-10 voyage of Oden to Pine Island Bay, West Antarctica, to investigate sea floor of Pine Island Trough using multibeam system and sediment cores. Small corrugation ridges within glacial furrows and lineations are thought to be imprint of last, semi-buoyant icebergs resulting from major break-up of Late Glacial Pine Island ice shelf.
Notes:

Polarforskningssecretariatet Årsbok = Swedish Polar Research Secretariat Yearbook. Vol. 2010 :24-27 (2011).

Keywords: 551.32 -- Glaciology.
551.336 -- Ice ages.
551.332.25 -- Glacio-marine deposits.
551.35 -- Marine sediments.
551.351 -- Coastal deposits.
551.324.22 -- Glaciers: Pine Island.
629.12 -- Vessels: Oden.
91(08) -- Expeditions: 1988- Swedish Antarctic Research Programme.
91(08) -- Expeditions: 2009-10 SWEDARP.
E5 -- Glaciology: land ice.
(*7) -- Antarctic regions.
(*7.7) -- West Antarctica.
(*77) -- Antarctica, Pacific sector.
(*772.9) -- Walgreen Coast.
(*80) -- Southern Ocean.
SPRI record no.: 199813

MARCXML

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100 1# ‡aJakobsson, Martin.
245 10 ‡aDet västantarktiska istäckets tillbakadragande efter den senaste istidens maximala utbredning = The retreat of the West Antarctic ice sheet since the last glacial maximum /‡cMartin Jakobsson, and 7 others.
260 ## ‡a[S.l.] :‡b[s.n.],‡c2011.
300 ## ‡ap. 24-27 :‡bill.
500 ## ‡aPolarforskningssecretariatet Årsbok = Swedish Polar Research Secretariat Yearbook. Vol. 2010 :24-27 (2011).
520 3# ‡aOverview of research during 2009-10 voyage of Oden to Pine Island Bay, West Antarctica, to investigate sea floor of Pine Island Trough using multibeam system and sediment cores. Small corrugation ridges within glacial furrows and lineations are thought to be imprint of last, semi-buoyant icebergs resulting from major break-up of Late Glacial Pine Island ice shelf.
650 07 ‡a551.32 -- Glaciology.‡2udc
650 07 ‡a551.336 -- Ice ages.‡2udc
650 07 ‡a551.332.25 -- Glacio-marine deposits.‡2udc
650 07 ‡a551.35 -- Marine sediments.‡2udc
650 07 ‡a551.351 -- Coastal deposits.‡2udc
650 07 ‡a551.324.22 -- Glaciers: Pine Island.‡2udc
650 07 ‡a629.12 -- Vessels: Oden.‡2udc
650 07 ‡a91(08) -- Expeditions: 1988- Swedish Antarctic Research Programme.‡2udc
650 07 ‡a91(08) -- Expeditions: 2009-10 SWEDARP.‡2udc
650 07 ‡aE5 -- Glaciology: land ice.‡2local
651 #7 ‡a(*7) -- Antarctic regions.‡2udc
651 #7 ‡a(*7.7) -- West Antarctica.‡2udc
651 #7 ‡a(*77) -- Antarctica, Pacific sector.‡2udc
651 #7 ‡a(*772.9) -- Walgreen Coast.‡2udc
651 #7 ‡a(*80) -- Southern Ocean.‡2udc
773 0# ‡7nnas ‡tPolarforskningssecretariatet Årsbok = Swedish Polar Research Secretariat Yearbook. ‡gVol. 2010 (2011) ‡wSPRI-145705
916 ## ‡a2012/07/17 -- HS
917 ## ‡aUnenhanced record from Muscat, imported 2019
948 3# ‡a20220924 ‡bHS