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Record #112074:
- #112074
Main publication details
MARC recordIce-deformation processes from mapping of c-axis fabrics / Anthony J. Gow, Richard B. Alley, Debra A. Meese.
| Title: | Ice-deformation processes from mapping of c-axis fabrics / Anthony J. Gow, Richard B. Alley, Debra A. Meese. |
| Author(s): | Gow, Anthony J. Alley, Richard B. Meese, Debra A. |
| Date: | 1991. |
| In: | Eos : transactions, American Geophysical Union. (1991.), Vol. 72(44, supplement) (1991) |
| Abstract: | AGU Fall Meeting Program and Abstracts, December 9-13, 1991. In Byrd station ice core, grain size increased down to 400 m depth but remained constant over next several hundred metres. Discusses possible mechanisms to stop grain growth. Preliminary measurements show that c-axes in ice from shallower than 400 m in Byrd core have random nearest-neighbour relations, but that deeper ice has non-random fabric with many small misorientations. It thus appears that polygonization causes grain growth to stop there, below 400 m. |
| Notes: | Eos : transactions, American Geophysical Union. Vol. 72(44, supplement) :150 (1991). |
| Keywords: | 551.32 -- Glaciology. 551.324 -- Land ice. 551.324.2 -- Types of land ice. 551.324.8 -- Land ice, structure and surface features. 551.321.2 -- Snow and ice, methods of sampling, excavating, drilling, etc. 622.14 -- Core sampling, ice and snow. 548.2 -- Ice, granular structure. Anisotropy. 548.53 -- Ice, recrystallization and grain growth. E5 -- Glaciology: land ice. (*7) -- Antarctic regions. (*772) -- Byrd Land. |
| SPRI record no.: | 112074 |
LDR 01793naa#a2200000#a#4500 001 SPRI-112074 005 20230323045254.0 007 ta 008 230323s1991####xx####|##|###|0||#0|eng#d 035 ## ‡aSPRI-112074 040 ## ‡aUkCU-P‡beng‡eaacr 100 1# ‡aGow, Anthony J. 245 10 ‡aIce-deformation processes from mapping of c-axis fabrics /‡cAnthony J. Gow, Richard B. Alley, Debra A. Meese. 260 ## ‡a[S.l.] :‡b[s.n.],‡c1991. 300 ## ‡ap. 150. 500 ## ‡aEos : transactions, American Geophysical Union. Vol. 72(44, supplement) :150 (1991). 520 3# ‡aAGU Fall Meeting Program and Abstracts, December 9-13, 1991. In Byrd station ice core, grain size increased down to 400 m depth but remained constant over next several hundred metres. Discusses possible mechanisms to stop grain growth. Preliminary measurements show that c-axes in ice from shallower than 400 m in Byrd core have random nearest-neighbour relations, but that deeper ice has non-random fabric with many small misorientations. It thus appears that polygonization causes grain growth to stop there, below 400 m. 650 07 ‡a551.32 -- Glaciology.‡2udc 650 07 ‡a551.324 -- Land ice.‡2udc 650 07 ‡a551.324.2 -- Types of land ice.‡2udc 650 07 ‡a551.324.8 -- Land ice, structure and surface features.‡2udc 650 07 ‡a551.321.2 -- Snow and ice, methods of sampling, excavating, drilling, etc.‡2udc 650 07 ‡a622.14 -- Core sampling, ice and snow.‡2udc 650 07 ‡a548.2 -- Ice, granular structure. Anisotropy.‡2udc 650 07 ‡a548.53 -- Ice, recrystallization and grain growth.‡2udc 650 07 ‡aE5 -- Glaciology: land ice.‡2local 651 #7 ‡a(*7) -- Antarctic regions.‡2udc 651 #7 ‡a(*772) -- Byrd Land.‡2udc 700 1# ‡aAlley, Richard B. 700 1# ‡aMeese, Debra A. 773 0# ‡7nnas ‡tEos : transactions, American Geophysical Union. ‡gVol. 72(44, supplement) (1991) ‡wSPRI-1028 917 ## ‡aUnenhanced record from Muscat, imported 2019 948 3# ‡a20230323