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Record #131398:

The Eemian and Weichselian stratigraphy of the Langelandselv area, Jameson Land, East Greenland / Jon Y. Landvik, Astrid Lyså, Svend Funder, Michael Kelly.

Title: The Eemian and Weichselian stratigraphy of the Langelandselv area, Jameson Land, East Greenland / Jon Y. Landvik, Astrid Lyså, Svend Funder, Michael Kelly.
Author(s): Landvik, Jon Y.
Lyså, Astrid.
Funder, Svend.
Kelly, Michael.
Date: 1994.
In: Boreas. (1994.), Vol. 23(4) (1994)
Abstract: Coastal Jameson Land is characterized by thick Quaternary deposits from last interglacial/glacial cycle. Successions at mouth of Langelandselv exhibit key stratigraphy where sediments from its interglaciation (Eemian) are overlain by three till units interbedded with glacimarine and deltaic interstadial successions. Immediately after retreat of glaciers after Saalian glaciation, warm Atlantic water surpassed what is known from Holocene. Two tills reflect readvances of fjord glaciers. Dates are suggested for interstades.
Notes:

Boreas. Vol. 23(4) :412-423 (1994).

Keywords: 551.1/.4 -- Geology.
551.3.051 -- Sedimentation and stratification.
551.324.6 -- Land ice, fluctuation.
551.332.21 -- Till or boulder clay. Tillite. Glacial diamictites.
551.336 -- Ice ages.
551.7 -- Stratigraphy.
551.79 -- Quaternary.
B -- Geology and soil sciences.
(*3) -- Arctic regions.
(*38) -- Greenland.
(*381) -- East Greenland.
(*381.4) -- Kong Christian den Xs Land.
SPRI record no.: 131398

MARCXML

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001 SPRI-131398
005 20190822084731.0
007 ta
008 190822s1994####xx#ab#|##|###|0||#0|eng#d
035 ## ‡aSPRI-131398
035 ## ‡a(UkCU)-depfacozdb
040 ## ‡aUkCU-P‡beng‡eaacr
245 04 ‡aThe Eemian and Weichselian stratigraphy of the Langelandselv area, Jameson Land, East Greenland /‡cJon Y. Landvik, Astrid Lyså, Svend Funder, Michael Kelly.
260 ## ‡a[S.l.] :‡b[s.n.],‡c1994.
300 ## ‡ap. 412-423 :‡bill., diags., tables, map.
500 ## ‡aBoreas. Vol. 23(4) :412-423 (1994).
520 3# ‡aCoastal Jameson Land is characterized by thick Quaternary deposits from last interglacial/glacial cycle. Successions at mouth of Langelandselv exhibit key stratigraphy where sediments from its interglaciation (Eemian) are overlain by three till units interbedded with glacimarine and deltaic interstadial successions. Immediately after retreat of glaciers after Saalian glaciation, warm Atlantic water surpassed what is known from Holocene. Two tills reflect readvances of fjord glaciers. Dates are suggested for interstades.
650 07 ‡a551.1/.4 -- Geology.‡2udc
650 07 ‡a551.3.051 -- Sedimentation and stratification.‡2udc
650 07 ‡a551.324.6 -- Land ice, fluctuation.‡2udc
650 07 ‡a551.332.21 -- Till or boulder clay. Tillite. Glacial diamictites.‡2udc
650 07 ‡a551.336 -- Ice ages.‡2udc
650 07 ‡a551.7 -- Stratigraphy.‡2udc
650 07 ‡a551.79 -- Quaternary.‡2udc
650 07 ‡aB -- Geology and soil sciences.‡2local
651 #7 ‡a(*3) -- Arctic regions.‡2udc
651 #7 ‡a(*38) -- Greenland.‡2udc
651 #7 ‡a(*381) -- East Greenland.‡2udc
651 #7 ‡a(*381.4) -- Kong Christian den Xs Land.‡2udc
700 1# ‡aLandvik, Jon Y.
700 1# ‡aLyså, Astrid.
700 1# ‡aFunder, Svend.
700 1# ‡aKelly, Michael.
773 0# ‡7nnas ‡tBoreas. ‡gVol. 23(4) (1994) ‡wSPRI-56035
917 ## ‡aTEST RECORD FROM MUSCAT: β4 ‡aUnenhanced record from Muscat, imported 2019
948 3# ‡a20190822