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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 |
LDR 01560naa#a2200000#a#4500 001 SPRI-131397 005 20240329132104.0 007 ta 008 240329s1994####xx#ab#|##|###|0||#0|eng#d 035 ## ‡aSPRI-131397 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 ## ‡aUnenhanced record from Muscat, imported 2019 948 3# ‡a20240329