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Record #126654:

Thermoluminescence profiles in meteorite finds, climatic change, and ice thicknesses in the Allan Hills, Antarctica, during the Quaternary / Paul H. Benoit, Derek W.G. Sears.

Title: Thermoluminescence profiles in meteorite finds, climatic change, and ice thicknesses in the Allan Hills, Antarctica, during the Quaternary / Paul H. Benoit, Derek W.G. Sears.
Author(s): Benoit, Paul H.
Sears, Derek W. G.
Date: 1993[pub.1994]
In: Antarctic Journal of the United States. (1993[pub.1994]), Vol. 28(5) (1993[pub.1994])
Abstract: There is some question as to how central Antarctic ice sheet, as opposed to outlet glaciers and ice of Ross embayment, has responded to climatic variation. Terrestrial thermal profiles of one particular meteorite were examined, as this is related to its terrestrial age and thermal history, and implications for icefield on which it was found are discussed. Concludes that ice thickness of this region has been within few 100 m of present value over last 100 ka, despite glacial--interglacial cycles.
Notes:

Antarctic Journal of the United States. Vol. 28(5) :52-54 (1993[pub.1994]).

Keywords: 551.336 -- Ice ages.
551.79 -- Quaternary.
551.583.3 -- Climatic changes, Quaternary.
551.588.5 -- Climate, relationship with ice.
552.6 -- Meteorites, petrological aspects.
91(08) -- Expeditions: 1955- US Antarctic Program.
E7 -- Glaciology: glacial geology and ice ages.
(*7) -- Antarctic regions.
(*749.5) -- Transantarctic Mountains, Victoria Land.
SPRI record no.: 126654

MARCXML

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100 1# ‡aBenoit, Paul H.
245 10 ‡aThermoluminescence profiles in meteorite finds, climatic change, and ice thicknesses in the Allan Hills, Antarctica, during the Quaternary /‡cPaul H. Benoit, Derek W.G. Sears.
260 ## ‡a[S.l.] :‡b[s.n.],‡c1993[pub.1994]
300 ## ‡ap. 52-54 :‡bdiags.
500 ## ‡aAntarctic Journal of the United States. Vol. 28(5) :52-54 (1993[pub.1994]).
520 3# ‡aThere is some question as to how central Antarctic ice sheet, as opposed to outlet glaciers and ice of Ross embayment, has responded to climatic variation. Terrestrial thermal profiles of one particular meteorite were examined, as this is related to its terrestrial age and thermal history, and implications for icefield on which it was found are discussed. Concludes that ice thickness of this region has been within few 100 m of present value over last 100 ka, despite glacial--interglacial cycles.
650 07 ‡a551.336 -- Ice ages.‡2udc
650 07 ‡a551.79 -- Quaternary.‡2udc
650 07 ‡a551.583.3 -- Climatic changes, Quaternary.‡2udc
650 07 ‡a551.588.5 -- Climate, relationship with ice.‡2udc
650 07 ‡a552.6 -- Meteorites, petrological aspects.‡2udc
650 07 ‡a91(08) -- Expeditions: 1955- US Antarctic Program.‡2udc
650 07 ‡aE7 -- Glaciology: glacial geology and ice ages.‡2local
651 #7 ‡a(*7) -- Antarctic regions.‡2udc
651 #7 ‡a(*749.5) -- Transantarctic Mountains, Victoria Land.‡2udc
700 1# ‡aSears, Derek W. G.
773 0# ‡7nnas ‡tAntarctic Journal of the United States. ‡gVol. 28(5) (1993[pub.1994]) ‡wSPRI-41791
917 ## ‡aUnenhanced record from Muscat, imported 2019
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