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Record #125057:

Texture and fabrics in the GRIP ice core: implication for ice deformation and the climatic record / T. Thorsteinsson, S. Kipfstuhl, H. Eicken.

Title: Texture and fabrics in the GRIP ice core: implication for ice deformation and the climatic record / T. Thorsteinsson, S. Kipfstuhl, H. Eicken.
Author(s): Thorsteinsson, T.
Kipfstuhl, S.
Eicken, H.
Date: 1993.
In: Eos : transactions, American Geophysical Union. (1993.), Vol. 74(43, supplement) (1993)
Abstract: Abstract. Results from c-axis orientation measurements on 3029 m long Greenland Ice-core Project (GRIP) ice core from central Greenland show progressive downward strengthening of fabric from random to single maximum and confirm that vertical compression is main mode of deformation down to 2850 m. Below that, elongation of single maximum was observed, suggesting presence of longitudinal stress. Very large crystals are seen in lower 100 m.
Notes:

Eos : transactions, American Geophysical Union. Vol. 74(43, supplement) :84 (1993).

Keywords: 551.32 -- Glaciology.
551.324 -- Land ice.
551.324.24 -- Ice sheets and caps.
551.321.2 -- Snow and ice, methods of sampling, excavating, drilling, etc.
622.14 -- Core sampling, ice and snow.
548 -- Crystallography.
551.324.8 -- Land ice, structure and surface features.
539.37 -- Ice, plastic and viscous deformation.
001.89 -- Research programmes: Greenland Ice-core Project (GRIP).
551.58 -- Climatology.
551.583 -- Climatic changes.
E5 -- Glaciology: land ice.
(*38) -- Greenland.
SPRI record no.: 125057

MARCXML

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100 1# ‡aThorsteinsson, T.
245 10 ‡aTexture and fabrics in the GRIP ice core :‡bimplication for ice deformation and the climatic record /‡cT. Thorsteinsson, S. Kipfstuhl, H. Eicken.
260 ## ‡a[S.l.] :‡b[s.n.],‡c1993.
300 ## ‡ap. 84.
500 ## ‡aEos : transactions, American Geophysical Union. Vol. 74(43, supplement) :84 (1993).
520 3# ‡aAbstract. Results from c-axis orientation measurements on 3029 m long Greenland Ice-core Project (GRIP) ice core from central Greenland show progressive downward strengthening of fabric from random to single maximum and confirm that vertical compression is main mode of deformation down to 2850 m. Below that, elongation of single maximum was observed, suggesting presence of longitudinal stress. Very large crystals are seen in lower 100 m.
650 07 ‡a551.32 -- Glaciology.‡2udc
650 07 ‡a551.324 -- Land ice.‡2udc
650 07 ‡a551.324.24 -- Ice sheets and caps.‡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 -- Crystallography.‡2udc
650 07 ‡a551.324.8 -- Land ice, structure and surface features.‡2udc
650 07 ‡a539.37 -- Ice, plastic and viscous deformation.‡2udc
650 07 ‡a001.89 -- Research programmes: Greenland Ice-core Project (GRIP).‡2udc
650 07 ‡a551.58 -- Climatology.‡2udc
650 07 ‡a551.583 -- Climatic changes.‡2udc
650 07 ‡aE5 -- Glaciology: land ice.‡2local
651 #7 ‡a(*38) -- Greenland.‡2udc
700 1# ‡aKipfstuhl, S.
700 1# ‡aEicken, H.
773 0# ‡7nnas ‡tEos : transactions, American Geophysical Union. ‡gVol. 74(43, supplement) (1993) ‡wSPRI-1028
917 ## ‡aUnenhanced record from Muscat, imported 2019
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