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Record #155452:
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Main publication details
MARC recordBehaviour of subglacial sediment and basal ice in a cold glacier / Sean J. Fitzsimons, R.D. (Reginald D.) Lorrain, Marcus J. Vandergoes.
| Title: | Behaviour of subglacial sediment and basal ice in a cold glacier / Sean J. Fitzsimons, R.D. (Reginald D.) Lorrain, Marcus J. Vandergoes. |
| Author(s): | Fitzsimons, Sean J. Lorrain, R. D. Vandergoes, Marcus J. |
| Date: | 2000. |
| Publisher: | London: Geological Society |
| In: | Deformation of glacial materials. (2000.), |
| Abstract: | Measurements made in tunnel into bed of Suess Glacier, Taylor Valley, Antarctica over two years of ice velocity, taken with glaciotectonic structures, show distinct strain concentration, sliding interface and thin shear zones of planes within basal ice. Highest strain rates occur in amber ice. Suggests shear strength is controlled by ice chemistry and debris concentration. |
| Notes: | In: Deformation of glacial materials / Alex J. Maltman, Bryn Hubbard, Michael J. Hambrey, eds. |
| Keywords: | 551.32 -- Glaciology. 551.324.2 -- Types of land ice. 551.324.22 -- Glaciers: Suess Glacier. 551.33 -- Glacial geology. 551.331.5 -- Glacial erosion and protection. Sub-glacial topography. 551.333 -- Glacial deformation and glaciotectonic structures. E7 -- Glaciology: glacial geology and ice ages. (*7) -- Antarctic regions. (*762.4) -- Scott Coast. |
| SPRI record no.: | 155452 |
LDR 01702naa#a2200000#a#4500 001 SPRI-155452 005 20240419084520.0 007 ta 008 240419s2000####enka###|#####|0||#0#eng#d 035 ## ‡aSPRI-155452 040 ## ‡aUkCU-P‡beng‡eaacr 100 1# ‡aFitzsimons, Sean J. 245 10 ‡aBehaviour of subglacial sediment and basal ice in a cold glacier /‡cSean J. Fitzsimons, R.D. (Reginald D.) Lorrain, Marcus J. Vandergoes. 260 ## ‡aLondon :‡bGeological Society,‡c2000. 300 ## ‡ap. 181-190 :‡bill., diags., table. 500 ## ‡aIn: Deformation of glacial materials / Alex J. Maltman, Bryn Hubbard, Michael J. Hambrey, eds. 520 3# ‡aMeasurements made in tunnel into bed of Suess Glacier, Taylor Valley, Antarctica over two years of ice velocity, taken with glaciotectonic structures, show distinct strain concentration, sliding interface and thin shear zones of planes within basal ice. Highest strain rates occur in amber ice. Suggests shear strength is controlled by ice chemistry and debris concentration. 650 07 ‡a551.32 -- Glaciology.‡2udc 650 07 ‡a551.324.2 -- Types of land ice.‡2udc 650 07 ‡a551.324.22 -- Glaciers: Suess Glacier.‡2udc 650 07 ‡a551.33 -- Glacial geology.‡2udc 650 07 ‡a551.331.5 -- Glacial erosion and protection. Sub-glacial topography.‡2udc 650 07 ‡a551.333 -- Glacial deformation and glaciotectonic structures.‡2udc 650 07 ‡aE7 -- Glaciology: glacial geology and ice ages.‡2local 651 #7 ‡a(*7) -- Antarctic regions.‡2udc 651 #7 ‡a(*762.4) -- Scott Coast.‡2udc 700 1# ‡aLorrain, R. D. ‡q(Reginald D. ) 700 1# ‡aVandergoes, Marcus J. 773 0# ‡7nnam ‡aAlex J. Maltman, Bryn Hubbard, Michael J. Hambrey, eds. ‡tDeformation of glacial materials. ‡dLondon : Geological Society, 2000. ‡wSPRI-154378 917 ## ‡aUnenhanced record from Muscat, imported 2019 948 3# ‡a20240419