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Record #118490:
- #118490
Main publication details
MARC recordThe last interglacial--glacial period on Spitsbergen, Svalbard / Jan Mangerud, John Inge Svendsen.
| Title: | The last interglacial--glacial period on Spitsbergen, Svalbard / Jan Mangerud, John Inge Svendsen. |
| Author(s): | Mangerud, Jan. Svendsen, John Inge. |
| Date: | 1992. |
| In: | Quaternary Science Reviews. (1992.), Vol. 11(6) (1992) |
| Abstract: | Glaciation history of this Eemian--Weichselian (130 ka) period of Svalbard and north-west Barents Sea is reconstructed, based on studies of sediments exposed in coastal cliffs at head of Isfjorden. Four till beds separated by marine sediments are recognized, reflecting different climatic conditions. Postulated that Quaternary glaciations of Svalbard were driven by orbital variations with 41 ka tilt period, in contrast to Scandinavian glaciations that were partly driven by precession cycle with periodicity of 23 ka. |
| Notes: | Quaternary Science Reviews. Vol. 11(6) :633-664 (1992). |
| Keywords: | 551.33 -- Glacial geology. 551.336 -- Ice ages. 551.79 -- Quaternary. 551.332.25 -- Glacio-marine deposits. 551.332.212 -- Till or boulder clay. 551.583.3 -- Climatic changes, Quaternary. E7 -- Glaciology: glacial geology and ice ages. (*32) -- Svalbard. (*324) -- Spitsbergen. (*60) -- Arctic Ocean and adjacent waters. (*686) -- Barents Sea. |
| SPRI record no.: | 118490 |
LDR 01657naa#a2200000#a#4500 001 SPRI-118490 005 20240417002438.0 007 ta 008 240417s1992####xx#ab#|##|###|0||#0|eng#d 035 ## ‡aSPRI-118490 040 ## ‡aUkCU-P‡beng‡eaacr 100 1# ‡aMangerud, Jan. 245 14 ‡aThe last interglacial--glacial period on Spitsbergen, Svalbard /‡cJan Mangerud, John Inge Svendsen. 260 ## ‡a[S.l.] :‡b[s.n.],‡c1992. 300 ## ‡ap. 633-664 :‡bill., diags., tables, maps. 500 ## ‡aQuaternary Science Reviews. Vol. 11(6) :633-664 (1992). 520 3# ‡aGlaciation history of this Eemian--Weichselian (130 ka) period of Svalbard and north-west Barents Sea is reconstructed, based on studies of sediments exposed in coastal cliffs at head of Isfjorden. Four till beds separated by marine sediments are recognized, reflecting different climatic conditions. Postulated that Quaternary glaciations of Svalbard were driven by orbital variations with 41 ka tilt period, in contrast to Scandinavian glaciations that were partly driven by precession cycle with periodicity of 23 ka. 650 07 ‡a551.33 -- Glacial geology.‡2udc 650 07 ‡a551.336 -- Ice ages.‡2udc 650 07 ‡a551.79 -- Quaternary.‡2udc 650 07 ‡a551.332.25 -- Glacio-marine deposits.‡2udc 650 07 ‡a551.332.212 -- Till or boulder clay.‡2udc 650 07 ‡a551.583.3 -- Climatic changes, Quaternary.‡2udc 650 07 ‡aE7 -- Glaciology: glacial geology and ice ages.‡2local 651 #7 ‡a(*32) -- Svalbard.‡2udc 651 #7 ‡a(*324) -- Spitsbergen.‡2udc 651 #7 ‡a(*60) -- Arctic Ocean and adjacent waters.‡2udc 651 #7 ‡a(*686) -- Barents Sea.‡2udc 700 1# ‡aSvendsen, John Inge. 773 0# ‡7nnas ‡tQuaternary Science Reviews. ‡gVol. 11(6) (1992) ‡wSPRI-78722 917 ## ‡aUnenhanced record from Muscat, imported 2019 948 3# ‡a20240417