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Record #122825:
Basal ice accretion and debris entrainment within the coastal ice margin, Law Dome, Antarctica / Ian D. Goodwin.
Title: | Basal ice accretion and debris entrainment within the coastal ice margin, Law Dome, Antarctica / Ian D. Goodwin. |
Author(s): | Goodwin, Ian D. |
Date: | 1993. |
In: | Journal of Glaciology. (1993.), Vol. 39(131) (1993) |
Abstract: | Study carried out in 1985 and 1987 revealed basal accretion of clean and debris-bearing ice, marine congelation and granular marine ice inland of margin. Co-isotopic analysis and solute chemistry were applied to determine modes of accretion and entrainment. Marine congelation ice and granular marine ice were formed, respectively, from basal freezing of desalinated sea water and episodic mixture of basal meltwater and sea water. Debris-banded ice with debris concentrations of 6.3 to 33% by volume was formed from proglacial raised beach and shallow marine sediment incorporated by overriding advance of ice margin. Debris-poor ice and laminated debris ice (0.9 to 1.9% by volume) were accreted further inland by basal regelation processes. |
Notes: | Journal of Glaciology. Vol. 39(131) :157-166 (1993). |
Keywords: | 551.32 -- Glaciology. 551.324 -- Land ice. 551.324.29 -- Land ice, miscellaneous forms. 551.324.83 -- Land ice, load: Law Dome. E5 -- Glaciology: land ice. (*7) -- Antarctic regions. (*747.3) -- Budd Coast. |
SPRI record no.: | 122825 |
LDR 01657naa#a2200000#a#4500 001 SPRI-122825 005 20231128154257.0 007 ta 008 231128s1993####xx#ab#|##|###|0||#0|eng#d 035 ## ‡aSPRI-122825 040 ## ‡aUkCU-P‡beng‡eaacr 100 1# ‡aGoodwin, Ian D. 245 10 ‡aBasal ice accretion and debris entrainment within the coastal ice margin, Law Dome, Antarctica /‡cIan D. Goodwin. 260 ## ‡a[S.l.] :‡b[s.n.],‡c1993. 300 ## ‡ap. 157-166 :‡bill., diags., map. 500 ## ‡aJournal of Glaciology. Vol. 39(131) :157-166 (1993). 520 3# ‡aStudy carried out in 1985 and 1987 revealed basal accretion of clean and debris-bearing ice, marine congelation and granular marine ice inland of margin. Co-isotopic analysis and solute chemistry were applied to determine modes of accretion and entrainment. Marine congelation ice and granular marine ice were formed, respectively, from basal freezing of desalinated sea water and episodic mixture of basal meltwater and sea water. Debris-banded ice with debris concentrations of 6.3 to 33% by volume was formed from proglacial raised beach and shallow marine sediment incorporated by overriding advance of ice margin. Debris-poor ice and laminated debris ice (0.9 to 1.9% by volume) were accreted further inland by basal regelation processes. 650 07 ‡a551.32 -- Glaciology.‡2udc 650 07 ‡a551.324 -- Land ice.‡2udc 650 07 ‡a551.324.29 -- Land ice, miscellaneous forms.‡2udc 650 07 ‡a551.324.83 -- Land ice, load: Law Dome.‡2udc 650 07 ‡aE5 -- Glaciology: land ice.‡2local 651 #7 ‡a(*7) -- Antarctic regions.‡2udc 651 #7 ‡a(*747.3) -- Budd Coast.‡2udc 773 0# ‡7nnas ‡tJournal of Glaciology. ‡gVol. 39(131) (1993) ‡wSPRI-20534 917 ## ‡aUnenhanced record from Muscat, imported 2019 948 3# ‡a20231128