Distribution of Narrow-Width Magnetic Anomalies in Antarctica
Data for aeromagnetic profiles obtained in Antarctica during the 1963-64 austral summer were used together with earlier results to construct a map showing the areal distribution of narrow-width magnetic anomalies. Numerous anomalies are associated with known volcanic mountains in western Antarctica....
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American Association for the Advancement of Science (AAAS)
1964
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craaas:10.1126/science.144.3621.993 2024-09-15T17:43:57+00:00 Distribution of Narrow-Width Magnetic Anomalies in Antarctica Behrendt, John C. 1964 http://dx.doi.org/10.1126/science.144.3621.993 https://www.science.org/doi/pdf/10.1126/science.144.3621.993 en eng American Association for the Advancement of Science (AAAS) Science volume 144, issue 3621, page 993-999 ISSN 0036-8075 1095-9203 journal-article 1964 craaas https://doi.org/10.1126/science.144.3621.993 2024-07-25T04:00:26Z Data for aeromagnetic profiles obtained in Antarctica during the 1963-64 austral summer were used together with earlier results to construct a map showing the areal distribution of narrow-width magnetic anomalies. Numerous anomalies are associated with known volcanic mountains in western Antarctica. A large area of few anomalies is probably a result of an extension of the thick metasedimentary section observed in the Ellsworth Mountains. Portions of the Trans-Antarctic Mountains have associated anomalies which are probably caused by late Cenozoic volcanic rocks. Article in Journal/Newspaper Antarc* Antarctic Antarctica AAAS Resource Center (American Association for the Advancement of Science) Science 144 3621 993 995 |
institution |
Open Polar |
collection |
AAAS Resource Center (American Association for the Advancement of Science) |
op_collection_id |
craaas |
language |
English |
description |
Data for aeromagnetic profiles obtained in Antarctica during the 1963-64 austral summer were used together with earlier results to construct a map showing the areal distribution of narrow-width magnetic anomalies. Numerous anomalies are associated with known volcanic mountains in western Antarctica. A large area of few anomalies is probably a result of an extension of the thick metasedimentary section observed in the Ellsworth Mountains. Portions of the Trans-Antarctic Mountains have associated anomalies which are probably caused by late Cenozoic volcanic rocks. |
format |
Article in Journal/Newspaper |
author |
Behrendt, John C. |
spellingShingle |
Behrendt, John C. Distribution of Narrow-Width Magnetic Anomalies in Antarctica |
author_facet |
Behrendt, John C. |
author_sort |
Behrendt, John C. |
title |
Distribution of Narrow-Width Magnetic Anomalies in Antarctica |
title_short |
Distribution of Narrow-Width Magnetic Anomalies in Antarctica |
title_full |
Distribution of Narrow-Width Magnetic Anomalies in Antarctica |
title_fullStr |
Distribution of Narrow-Width Magnetic Anomalies in Antarctica |
title_full_unstemmed |
Distribution of Narrow-Width Magnetic Anomalies in Antarctica |
title_sort |
distribution of narrow-width magnetic anomalies in antarctica |
publisher |
American Association for the Advancement of Science (AAAS) |
publishDate |
1964 |
url |
http://dx.doi.org/10.1126/science.144.3621.993 https://www.science.org/doi/pdf/10.1126/science.144.3621.993 |
genre |
Antarc* Antarctic Antarctica |
genre_facet |
Antarc* Antarctic Antarctica |
op_source |
Science volume 144, issue 3621, page 993-999 ISSN 0036-8075 1095-9203 |
op_doi |
https://doi.org/10.1126/science.144.3621.993 |
container_title |
Science |
container_volume |
144 |
container_issue |
3621 |
container_start_page |
993 |
op_container_end_page |
995 |
_version_ |
1810491181249855488 |