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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Published in:Science
Main Authors: Anderson, John J., Bastien, Thomas W., Schmidt, Paul G., Splettstoesser, John F., Craddock, Campbell
Format: Article in Journal/Newspaper
Language:English
Published: American Association for the Advancement of Science (AAAS) 1962
Subjects:
Online Access:http://dx.doi.org/10.1126/science.138.3542.824
https://www.science.org/doi/pdf/10.1126/science.138.3542.824
id craaas:10.1126/science.138.3542.824
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spelling 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
institution Open Polar
collection 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
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