Continental Margins

Continental Margins

Author: National Research Council (U.S.). Ad Hoc Panel to Investigate the Geological and Geophysical Research Needs and Problems of Continental Margins

Publisher:

Published: 1979

Total Pages: 332

ISBN-13:

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Geology and Seismic Stratigraphy of the Antarctic Margin

Geology and Seismic Stratigraphy of the Antarctic Margin

Author: Alan K. Cooper

Publisher: American Geophysical Union

Published: 1997-01-23

Total Pages: 490

ISBN-13: 9780875908847

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Published by the American Geophysical Union as part of the Antarctic Research Series, Volume 71. The Antarctic Ice Sheet has greatly affected global climate, sea level, ocean circulation, and southern hemisphere biota during Cenozoic times. Much of our understanding of the evolution of the ice sheet has been inferred from isotopic studies on distant deep-ocean sediments, because few Cenozoic rocks are exposed on the Antarctic continent. Yet, large differences occur between past ice volumes inferred from isotopic studies and those inferred from low-latitude sea-level variation. The massive quantities of glacially transported terrigenous sediments that lie beneath the Antarctic continental margin provide an additional, more direct record of the inferred ice sheet fluctuations. Volume 68 addresses the history of ice sheet fluctuations as recorded by geological and geophysical investigations of selected areas of the Antarctic continental margin. As described below, the volume gives data and results from on-going research by a major multinational project directed toward better understanding the impact of Antarctic Ice Sheet fluctuations on global sea levels and climates.


Geology and Seismic Stratigraphy of the Antarctic Margin

Geology and Seismic Stratigraphy of the Antarctic Margin

Author: Alan K. Cooper

Publisher: Wiley-AGU

Published: 1997-01-23

Total Pages: 0

ISBN-13: 9781118658697

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The Antarctic Ice Sheet has greatly affected global climate, sea level, ocean circulation, and southern hemisphere biota during Cenozoic times. Much of our understanding of the evolution of the ice sheet has been inferred from isotopic studies on distant deep-ocean sediments, because few Cenozoic rocks are exposed on the Antarctic continent. Yet, large differences occur between past ice volumes inferred from isotopic studies and those inferred from low-latitude sea-level variation. The massive quantities of glacially transported terrigenous sediments that lie beneath the Antarctic continental margin provide an additional, more direct record of the inferred ice sheet fluctuations. Volume 68 addresses the history of ice sheet fluctuations as recorded by geological and geophysical investigations of selected areas of the Antarctic continental margin. As described below, the volume gives data and results from on-going research by a major multinational project directed toward better understanding the impact of Antarctic Ice Sheet fluctuations on global sea levels and climates.