Catastrophic ice shelf breakup as the source of Heinrich event icebergs-Reference-Cited by-同舟云学术

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Catastrophic ice shelf breakup as the source of Heinrich event icebergs

Published:2004-01-22 Issue:1 Volume:19 Page:n/a-n/a
ISSN:0883-8305
Container-title:Paleoceanography
language:en
Short-container-title:Paleoceanography

Author:

Hulbe Christina L.¹,MacAyeal Douglas R.²,Denton George H.³,Kleman Johan⁴,Lowell Thomas V.⁵

Affiliation:

1. Department of Geology; Portland State University; Portland; Oregon; USA

2. Department of the Geophysical Sciences; University of Chicago; Chicago; Illinois; USA

3. Institute for Quaternary and Climate Studies and Department of Geological Sciences; University of Maine; Orono; Maine; USA

4. Department of Physical Geography and Quaternary Geology; Stockholm University; Stockholm; Sweden

5. Department of Geology; University of Cincinnati; Cincinnati; Ohio; USA

Publisher

American Geophysical Union (AGU)

Subject

Paleontology,Oceanography

Reference98 articles.

1. Late Quaternary stratigraphy and paleoceanography of NW Labrador Sea;Aksu;Mar. Micropaleontol.,1985

2. Sedimentary deposits may cause fluctuations of tidewater glaciers;Alley;Ann. Glaciol.,1991

3. Ice-rafted debris associated with binge/purge oscillations of the Laurentide ice sheet;Alley;Paleoceanography,1994

4. Glaciohydraulic supercooling: A freeze-on mechanism to create stratified, debris-rich basal ice. 2. Theory;Alley;J. Glaciol,1998

5. Detrital carbonate-rich sediments, northwestern Labrador Sea: Implications for ice-sheet dynamics and iceberg rafting (Heinrich) events in the North Atlantic;Andrews;Geology,1992

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