Extent of the Antarctic Continent

Group velocities of earthquake-generated Love and Rayleigh waves for certain transantarctic paths are abnormally high when compared with data from other continents. For these paths, the data indicate that at most only three-fourths of the antarctic ice sheet is underlain by continent, the remaining...

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Bibliographic Details
Published in:Science
Main Authors: Press, Frank, Dewart, Gilbert
Format: Article in Journal/Newspaper
Language:English
Published: American Association for the Advancement of Science (AAAS) 1959
Subjects:
Antarctic
The Antarctic
Antarc*
Ice Sheet
Online Access:http://dx.doi.org/10.1126/science.129.3347.462
https://www.science.org/doi/pdf/10.1126/science.129.3347.462
id craaas:10.1126/science.129.3347.462
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spelling craaas:10.1126/science.129.3347.462 2024-06-09T07:39:25+00:00 Extent of the Antarctic Continent Press, Frank Dewart, Gilbert 1959 http://dx.doi.org/10.1126/science.129.3347.462 https://www.science.org/doi/pdf/10.1126/science.129.3347.462 en eng American Association for the Advancement of Science (AAAS) Science volume 129, issue 3347, page 462-463 ISSN 0036-8075 1095-9203 journal-article 1959 craaas https://doi.org/10.1126/science.129.3347.462 2024-05-16T12:54:07Z Group velocities of earthquake-generated Love and Rayleigh waves for certain transantarctic paths are abnormally high when compared with data from other continents. For these paths, the data indicate that at most only three-fourths of the antarctic ice sheet is underlain by continent, the remaining area being oceanic in structure. Article in Journal/Newspaper Antarc* Antarctic Ice Sheet AAAS Resource Center (American Association for the Advancement of Science) Antarctic The Antarctic Science 129 3347 462 463
institution Open Polar
collection AAAS Resource Center (American Association for the Advancement of Science)
op_collection_id craaas
language English
description Group velocities of earthquake-generated Love and Rayleigh waves for certain transantarctic paths are abnormally high when compared with data from other continents. For these paths, the data indicate that at most only three-fourths of the antarctic ice sheet is underlain by continent, the remaining area being oceanic in structure.
format Article in Journal/Newspaper
author Press, Frank
Dewart, Gilbert
spellingShingle Press, Frank
Dewart, Gilbert
Extent of the Antarctic Continent
author_facet Press, Frank
Dewart, Gilbert
author_sort Press, Frank
title Extent of the Antarctic Continent
title_short Extent of the Antarctic Continent
title_full Extent of the Antarctic Continent
title_fullStr Extent of the Antarctic Continent
title_full_unstemmed Extent of the Antarctic Continent
title_sort extent of the antarctic continent
publisher American Association for the Advancement of Science (AAAS)
publishDate 1959
url http://dx.doi.org/10.1126/science.129.3347.462
https://www.science.org/doi/pdf/10.1126/science.129.3347.462
geographic Antarctic
The Antarctic
geographic_facet Antarctic
The Antarctic
genre Antarc*
Antarctic
Ice Sheet
genre_facet Antarc*
Antarctic
Ice Sheet
op_source Science
volume 129, issue 3347, page 462-463
ISSN 0036-8075 1095-9203
op_doi https://doi.org/10.1126/science.129.3347.462
container_title Science
container_volume 129
container_issue 3347
container_start_page 462
op_container_end_page 463
_version_ 1801379349615607808

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