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Record #97139:

Glacial-marine sedimentation and Quaternary glacial history of Marguerite Bay, Antarctic Peninsula / Douglas S. Kennedy, John B. Anderson.

Title: Glacial-marine sedimentation and Quaternary glacial history of Marguerite Bay, Antarctic Peninsula / Douglas S. Kennedy, John B. Anderson.
Author(s): Kennedy, Douglas S.
Anderson, John B.
Date: 1989.
In: Quaternary Research. (1989.), Vol. 21(2) (1989)
Abstract: Area is well-situated to study specific scenarios of Late Wisconsin ice-sheet expansion and local nature of ice-sheet advance and retreat. Reconstruction based on seismic reflection data and piston cores obtained in 1985 and 1986. Reconstruction of glacial history since last glacial maximum shows grounded ice filling bay during Late Wisconsin. Rising sea level caused uncoupling of ice sheet and slow retreat of ice shelf throughout Holocene.
Notes:

Quaternary Research. Vol. 21(2) :255-276 (1989).

Antarctic issue, based on Symposium on the Antarctic Ice Sheet and the Southern Ocean held at the 12th Congress of the International Union for Quaternary Research in Ottawa, Canada, on 8 August 1987.

Keywords: 551.332.25 -- Glacio-marine deposits.
551.336 -- Ice ages.
551.79 -- Quaternary.
E7 -- Glaciology: glacial geology and ice ages.
(*80) -- Southern Ocean.
(*82) -- South Atlantic Ocean.
(*7) -- Antarctic regions.
(*726) -- Maritime Antarctic.
(*726.3) -- Antarctic Peninsula.
(*726.57) -- Fallieres Coast.
SPRI record no.: 97139

MARCXML

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100 1# ‡aKennedy, Douglas S.
245 10 ‡aGlacial-marine sedimentation and Quaternary glacial history of Marguerite Bay, Antarctic Peninsula /‡cDouglas S. Kennedy, John B. Anderson.
260 ## ‡a[S.l.] :‡b[s.n.],‡c1989.
300 ## ‡ap. 255-276 :‡bill., diags., tables, maps.
500 ## ‡aQuaternary Research. Vol. 21(2) :255-276 (1989).
500 ## ‡aAntarctic issue, based on Symposium on the Antarctic Ice Sheet and the Southern Ocean held at the 12th Congress of the International Union for Quaternary Research in Ottawa, Canada, on 8 August 1987.
520 3# ‡aArea is well-situated to study specific scenarios of Late Wisconsin ice-sheet expansion and local nature of ice-sheet advance and retreat. Reconstruction based on seismic reflection data and piston cores obtained in 1985 and 1986. Reconstruction of glacial history since last glacial maximum shows grounded ice filling bay during Late Wisconsin. Rising sea level caused uncoupling of ice sheet and slow retreat of ice shelf throughout Holocene.
650 07 ‡a551.332.25 -- Glacio-marine deposits.‡2udc
650 07 ‡a551.336 -- Ice ages.‡2udc
650 07 ‡a551.79 -- Quaternary.‡2udc
650 07 ‡aE7 -- Glaciology: glacial geology and ice ages.‡2local
651 #7 ‡a(*80) -- Southern Ocean.‡2udc
651 #7 ‡a(*82) -- South Atlantic Ocean.‡2udc
651 #7 ‡a(*7) -- Antarctic regions.‡2udc
651 #7 ‡a(*726) -- Maritime Antarctic.‡2udc
651 #7 ‡a(*726.3) -- Antarctic Peninsula.‡2udc
651 #7 ‡a(*726.57) -- Fallieres Coast.‡2udc
700 1# ‡aAnderson, John B.
773 0# ‡7nnas ‡tQuaternary Research. ‡gVol. 21(2) (1989) ‡wSPRI-46567
917 ## ‡aUnenhanced record from Muscat, imported 2019
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