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Record #131397:

Palaeoenvironments and changes in relative sea level during the last interglaciation at Langelandselv, Jameson Land, East Greenland / Henrik Vosgerau, and six others.

Title: Palaeoenvironments and changes in relative sea level during the last interglaciation at Langelandselv, Jameson Land, East Greenland / Henrik Vosgerau, and six others.
Author(s): Vosgerau, Henrik.
Date: 1994.
In: Boreas. (1994.), Vol. 23(4) (1994)
Abstract: Coastal cliffs and stream-cut sections at Langelandselv show 22 m thick sedimentary succession reflecting development of shallow marine and fluvial environments during last interglaciation, when sea level rose from 0 to 18 m. Interglacial succession ends with glaciotectonically dislocated fluvial sand, and is capped by alternating beds of lodgement till and fluvial sand, deposited during Early Weichselian. Article gives dating techniques used.
Notes:

Boreas. Vol. 23(4) :398-411 (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.
551.79 -- Quaternary.
B -- Geology and soil sciences.
(*3) -- Arctic regions.
(*38) -- Greenland.
(*381) -- East Greenland.
(*381.4) -- Kong Christian den Xs Land.
SPRI record no.: 131397

MARCXML

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001 SPRI-131397
005 20190824040042.0
007 ta
008 190824s1994####xx#ab#|##|###|0||#0|eng#d
035 ## ‡aSPRI-131397
035 ## ‡a(UkCU)-depfacozdb
040 ## ‡aUkCU-P‡beng‡eaacr
100 1# ‡aVosgerau, Henrik.
245 10 ‡aPalaeoenvironments and changes in relative sea level during the last interglaciation at Langelandselv, Jameson Land, East Greenland /‡cHenrik Vosgerau, and six others.
260 ## ‡a[S.l.] :‡b[s.n.],‡c1994.
300 ## ‡ap. 398-411 :‡bill., diags., tables, map.
500 ## ‡aBoreas. Vol. 23(4) :398-411 (1994).
520 3# ‡aCoastal cliffs and stream-cut sections at Langelandselv show 22 m thick sedimentary succession reflecting development of shallow marine and fluvial environments during last interglaciation, when sea level rose from 0 to 18 m. Interglacial succession ends with glaciotectonically dislocated fluvial sand, and is capped by alternating beds of lodgement till and fluvial sand, deposited during Early Weichselian. Article gives dating techniques used.
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 ‡a551.79 -- 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
773 0# ‡7nnas ‡tBoreas. ‡gVol. 23(4) (1994) ‡wSPRI-56035
917 ## ‡aTEST RECORD FROM MUSCAT: β4 ‡aUnenhanced record from Muscat, imported 2019
948 3# ‡a20190824