Antarctica: Geology of the Ellsworth Mountains
Geologic reconnaissance indicates that the Ellsworth Mountains consist mainly of thousands of feet of folded, slightly metamorphosed, clastic sedimentary rocks of unknown age. Three major stratigraphic units are recognized, but only fragmentary fossils have been found. The folding is asymmetric, ove...
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American Association for the Advancement of Science (AAAS)
1962
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Online Access: | http://dx.doi.org/10.1126/science.138.3542.824 https://www.science.org/doi/pdf/10.1126/science.138.3542.824 |
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craaas:10.1126/science.138.3542.824 2024-06-09T07:39:59+00:00 Antarctica: Geology of the Ellsworth Mountains Anderson, John J. Bastien, Thomas W. Schmidt, Paul G. Splettstoesser, John F. Craddock, Campbell 1962 http://dx.doi.org/10.1126/science.138.3542.824 https://www.science.org/doi/pdf/10.1126/science.138.3542.824 en eng American Association for the Advancement of Science (AAAS) Science volume 138, issue 3542, page 824-825 ISSN 0036-8075 1095-9203 journal-article 1962 craaas https://doi.org/10.1126/science.138.3542.824 2024-05-16T12:54:27Z Geologic reconnaissance indicates that the Ellsworth Mountains consist mainly of thousands of feet of folded, slightly metamorphosed, clastic sedimentary rocks of unknown age. Three major stratigraphic units are recognized, but only fragmentary fossils have been found. The folding is asymmetric, overturned, or recumbent; fold axes strike north, 10° to 20° west. Basic igneous sills occur in the northern Heritage Range. Article in Journal/Newspaper Antarc* Antarctica AAAS Resource Center (American Association for the Advancement of Science) Ellsworth Mountains ENVELOPE(-85.000,-85.000,-78.750,-78.750) Heritage Range ENVELOPE(-82.000,-82.000,-80.000,-80.000) Science 138 3542 824 825 |
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Open Polar |
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AAAS Resource Center (American Association for the Advancement of Science) |
op_collection_id |
craaas |
language |
English |
description |
Geologic reconnaissance indicates that the Ellsworth Mountains consist mainly of thousands of feet of folded, slightly metamorphosed, clastic sedimentary rocks of unknown age. Three major stratigraphic units are recognized, but only fragmentary fossils have been found. The folding is asymmetric, overturned, or recumbent; fold axes strike north, 10° to 20° west. Basic igneous sills occur in the northern Heritage Range. |
format |
Article in Journal/Newspaper |
author |
Anderson, John J. Bastien, Thomas W. Schmidt, Paul G. Splettstoesser, John F. Craddock, Campbell |
spellingShingle |
Anderson, John J. Bastien, Thomas W. Schmidt, Paul G. Splettstoesser, John F. Craddock, Campbell Antarctica: Geology of the Ellsworth Mountains |
author_facet |
Anderson, John J. Bastien, Thomas W. Schmidt, Paul G. Splettstoesser, John F. Craddock, Campbell |
author_sort |
Anderson, John J. |
title |
Antarctica: Geology of the Ellsworth Mountains |
title_short |
Antarctica: Geology of the Ellsworth Mountains |
title_full |
Antarctica: Geology of the Ellsworth Mountains |
title_fullStr |
Antarctica: Geology of the Ellsworth Mountains |
title_full_unstemmed |
Antarctica: Geology of the Ellsworth Mountains |
title_sort |
antarctica: geology of the ellsworth mountains |
publisher |
American Association for the Advancement of Science (AAAS) |
publishDate |
1962 |
url |
http://dx.doi.org/10.1126/science.138.3542.824 https://www.science.org/doi/pdf/10.1126/science.138.3542.824 |
long_lat |
ENVELOPE(-85.000,-85.000,-78.750,-78.750) ENVELOPE(-82.000,-82.000,-80.000,-80.000) |
geographic |
Ellsworth Mountains Heritage Range |
geographic_facet |
Ellsworth Mountains Heritage Range |
genre |
Antarc* Antarctica |
genre_facet |
Antarc* Antarctica |
op_source |
Science volume 138, issue 3542, page 824-825 ISSN 0036-8075 1095-9203 |
op_doi |
https://doi.org/10.1126/science.138.3542.824 |
container_title |
Science |
container_volume |
138 |
container_issue |
3542 |
container_start_page |
824 |
op_container_end_page |
825 |
_version_ |
1801383502164262912 |