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Record #152524:

Textures and fabrics in the Dome F (Antarctica) ice core / N. Azuma, and 6 others.

Title: Textures and fabrics in the Dome F (Antarctica) ice core / N. Azuma, and 6 others.
Author(s): Azuma, N.
Date: 1999.
In: Annals of Glaciology. (1999.), Vol. 29 (1999)
Abstract: Measures crystal c-axis orientations, sizes and shape with automatic ice-fabric analyzer. Studies textural and fabric development through 2500 m long core from Dome F, Antarctica. Size increases steadily with depth except at some levels where size suddenly decreases. Finds clear correlation between crystal size and δ¹⁸O values. c-axis orientation fabrics change with depth from random orientation pattern to strong vertical single maximum at 2500 m, similar to those from GRIP (Greenland) core. Indication is that nucleation-recrystallization does not take place at Dome F.
Notes:

Annals of Glaciology. Vol. 29 :163-168 (1999).

Sixth International Symposium on Antarctic Glaciology (ISAG-6), 5--9 September 1998, Lanzhou, China, T.H. Jacka (Editor)

Keywords: 551.32 -- Glaciology.
551.321.2 -- Snow and ice, methods of sampling, excavating, drilling, etc.
622.14 -- Core sampling, ice and snow.
551.322 -- Ice and snow.
548 -- Crystallography.
548.2 -- Ice, granular structure. Anisotropy.
551.578.46 -- Snow cover and snow patches.
551.324 -- Land ice: Dome F.
E4 -- Glaciology: physics and chemistry of ice.
(*7) -- Antarctic regions.
(*73) -- Dronning Maud Land.
SPRI record no.: 152524

MARCXML

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100 1# ‡aAzuma, N.
245 10 ‡aTextures and fabrics in the Dome F (Antarctica) ice core /‡cN. Azuma, and 6 others.
260 ## ‡a[S.l.] :‡b[s.n.],‡c1999.
300 ## ‡ap. 163-168 :‡bill., diags.
500 ## ‡aAnnals of Glaciology. Vol. 29 :163-168 (1999).
500 ## ‡aSixth International Symposium on Antarctic Glaciology (ISAG-6), 5--9 September 1998, Lanzhou, China, T.H. Jacka (Editor)
520 3# ‡aMeasures crystal c-axis orientations, sizes and shape with automatic ice-fabric analyzer. Studies textural and fabric development through 2500 m long core from Dome F, Antarctica. Size increases steadily with depth except at some levels where size suddenly decreases. Finds clear correlation between crystal size and δ¹⁸O values. c-axis orientation fabrics change with depth from random orientation pattern to strong vertical single maximum at 2500 m, similar to those from GRIP (Greenland) core. Indication is that nucleation-recrystallization does not take place at Dome F.
650 07 ‡a551.32 -- Glaciology.‡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 ‡a551.322 -- Ice and snow.‡2udc
650 07 ‡a548 -- Crystallography.‡2udc
650 07 ‡a548.2 -- Ice, granular structure. Anisotropy.‡2udc
650 07 ‡a551.578.46 -- Snow cover and snow patches.‡2udc
650 07 ‡a551.324 -- Land ice: Dome F.‡2udc
650 07 ‡aE4 -- Glaciology: physics and chemistry of ice.‡2local
651 #7 ‡a(*7) -- Antarctic regions.‡2udc
651 #7 ‡a(*73) -- Dronning Maud Land.‡2udc
773 0# ‡7nnas ‡tAnnals of Glaciology. ‡gVol. 29 (1999) ‡wSPRI-60773
917 ## ‡aUnenhanced record from Muscat, imported 2019
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