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Record #149189:

Crystal-size and microparticle record in the ice core from Dome Summit South, Law Dome, East Antarctica / Jun Li, T.H. Jacka, Vin Morgan.

Title: Crystal-size and microparticle record in the ice core from Dome Summit South, Law Dome, East Antarctica / Jun Li, T.H. Jacka, Vin Morgan.
Author(s): Li, Jun.
Jacka, T. H.
Morgan, Vin.
Date: 1998.
In: Annals of Glaciology. (1998.), Vol. 27 (1998)
Abstract: Results from investigation of crystal size and microparticle variations in 1196 m ice core from Dome Summit South (DSS) near summit of Law Dome, East Antarctica, show microparticle concentrations are low for ice deposited during Holocene. Highest microparticle concentration occurs around 1133 m where oxygen isotope ratios show greatest negative values, e.g. Last Glacial Maximum, and crystal size reduces sharply.
Notes:

Annals of Glaciology. Vol. 27 :343-348 (1998).

International Symposium on Antarctica and Global Change: Interactions and Impacts, W.F. Budd (Editor), 13--18 July 1997, Hobart, Tasmania, Australia.

Keywords: 551.32 -- Glaciology.
551.324 -- Land ice.
551.322 -- Ice and snow.
548 -- Crystallography.
551.321.2 -- Snow and ice, methods of sampling, excavating, drilling, etc.
622.14 -- Core sampling, ice and snow.
551.336 -- Ice ages.
551.794 -- Holocene.
E7 -- Glaciology: glacial geology and ice ages.
(*7) -- Antarctic regions.
(*7.3) -- East Antarctica.
(*747.3) -- Budd Coast.
SPRI record no.: 149189

MARCXML

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245 10 ‡aCrystal-size and microparticle record in the ice core from Dome Summit South, Law Dome, East Antarctica /‡cJun Li, T.H. Jacka, Vin Morgan.
260 ## ‡a[S.l.] :‡b[s.n.],‡c1998.
300 ## ‡ap. 343-348 :‡bill., diags.
500 ## ‡aAnnals of Glaciology. Vol. 27 :343-348 (1998).
500 ## ‡aInternational Symposium on Antarctica and Global Change: Interactions and Impacts, W.F. Budd (Editor), 13--18 July 1997, Hobart, Tasmania, Australia.
520 3# ‡aResults from investigation of crystal size and microparticle variations in 1196 m ice core from Dome Summit South (DSS) near summit of Law Dome, East Antarctica, show microparticle concentrations are low for ice deposited during Holocene. Highest microparticle concentration occurs around 1133 m where oxygen isotope ratios show greatest negative values, e.g. Last Glacial Maximum, and crystal size reduces sharply.
650 07 ‡a551.32 -- Glaciology.‡2udc
650 07 ‡a551.324 -- Land ice.‡2udc
650 07 ‡a551.322 -- Ice and snow.‡2udc
650 07 ‡a548 -- Crystallography.‡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 ‡a551.336 -- Ice ages.‡2udc
650 07 ‡a551.794 -- Holocene.‡2udc
650 07 ‡aE7 -- Glaciology: glacial geology and ice ages.‡2local
651 #7 ‡a(*7) -- Antarctic regions.‡2udc
651 #7 ‡a(*7.3) -- East Antarctica.‡2udc
651 #7 ‡a(*747.3) -- Budd Coast.‡2udc
700 1# ‡aJacka, T. H.
700 1# ‡aMorgan, Vin.
773 0# ‡7nnas ‡tAnnals of Glaciology. ‡gVol. 27 (1998) ‡wSPRI-60773
917 ## ‡aUnenhanced record from Muscat, imported 2019
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