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Record #104782:

Stable isotope studies on ice margins in the Thule area / Niels Reeh, Henrik Højmark Thomsen, Poul Frich, Henrik B. Clausen.

Title: Stable isotope studies on ice margins in the Thule area / Niels Reeh, Henrik Højmark Thomsen, Poul Frich, Henrik B. Clausen.
Author(s): Reeh, Niels.
Thomsen, Henrik Højmark.
Frich, Poul.
Clausen, Henrik B.
Date: 1990.
In: Meddelelser om Grønland. Geoscience. (1990.), Vol. 22 (1990)
Abstract: Main aim of research programme was to investigate to what extent stable isotope studies in marginal areas of inland ice and local ice caps could provide information about the dynamic and climatic history of ice sheet during last glacial/interglacial cycle. This did not succeed because ice of Weichselian origin was not found at sites investigated, but study demonstrated usefulness of technique in glaciological studies of ice margins. Isotopic signature of ice, in terms of mean value as well as variability, is characteristic for site of formation of ice and for its thermal and phase-change history since time of formation.
Notes:

Meddelelser om Grønland. Geoscience. Vol. 22 :47-56 (1990).

Keywords: 551.324.84 -- Land ice, impurities.
551.32 -- Glaciology.
551.324 -- Land ice.
539.155.2 -- Isotopic analysis.
551.336 -- Ice ages.
551.79 -- Quaternary.
551.583.3 -- Climatic changes, Quaternary.
E3 -- Glaciology: instruments and methods.
(*38) -- Greenland.
(*387.6) -- Avanersuaq/Thule region.
SPRI record no.: 104782

MARCXML

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245 00 ‡aStable isotope studies on ice margins in the Thule area /‡cNiels Reeh, Henrik Højmark Thomsen, Poul Frich, Henrik B. Clausen.
260 ## ‡a[S.l.] :‡b[s.n.],‡c1990.
300 ## ‡ap. 47-56 :‡bdiags., table, maps.
500 ## ‡aMeddelelser om Grønland. Geoscience. Vol. 22 :47-56 (1990).
520 3# ‡aMain aim of research programme was to investigate to what extent stable isotope studies in marginal areas of inland ice and local ice caps could provide information about the dynamic and climatic history of ice sheet during last glacial/interglacial cycle. This did not succeed because ice of Weichselian origin was not found at sites investigated, but study demonstrated usefulness of technique in glaciological studies of ice margins. Isotopic signature of ice, in terms of mean value as well as variability, is characteristic for site of formation of ice and for its thermal and phase-change history since time of formation.
650 07 ‡a551.324.84 -- Land ice, impurities.‡2udc
650 07 ‡a551.32 -- Glaciology.‡2udc
650 07 ‡a551.324 -- Land ice.‡2udc
650 07 ‡a539.155.2 -- Isotopic analysis.‡2udc
650 07 ‡a551.336 -- Ice ages.‡2udc
650 07 ‡a551.79 -- Quaternary.‡2udc
650 07 ‡a551.583.3 -- Climatic changes, Quaternary.‡2udc
650 07 ‡aE3 -- Glaciology: instruments and methods.‡2local
651 #7 ‡a(*38) -- Greenland.‡2udc
651 #7 ‡a(*387.6) -- Avanersuaq/Thule region.‡2udc
700 1# ‡aReeh, Niels.
700 1# ‡aThomsen, Henrik Højmark.
700 1# ‡aFrich, Poul.
700 1# ‡aClausen, Henrik B.
773 0# ‡7nnas ‡tMeddelelser om Grønland. Geoscience. ‡gVol. 22 (1990) ‡wSPRI-59086
917 ## ‡aUnenhanced record from Muscat, imported 2019
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