Sedimentary Rocks of the Buckeye Range, Horlick Mountains, Antarctica
In the Buckeye Range of the Horlick Mountains, 4000 feet of sedimentary rocks nonconformably overlie a granitic basement and underlie a thick diabasic sill. The sedimentary section consists of Devonian sandstone and shale (Horlick formation), Carboniferous (?) tillite (Buckeye formation), Permian (?...
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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.136.3513.319 https://www.science.org/doi/pdf/10.1126/science.136.3513.319 |
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craaas:10.1126/science.136.3513.319 2024-06-09T07:39:39+00:00 Sedimentary Rocks of the Buckeye Range, Horlick Mountains, Antarctica Long, William E. 1962 http://dx.doi.org/10.1126/science.136.3513.319 https://www.science.org/doi/pdf/10.1126/science.136.3513.319 en eng American Association for the Advancement of Science (AAAS) Science volume 136, issue 3513, page 319-321 ISSN 0036-8075 1095-9203 journal-article 1962 craaas https://doi.org/10.1126/science.136.3513.319 2024-05-16T12:55:36Z In the Buckeye Range of the Horlick Mountains, 4000 feet of sedimentary rocks nonconformably overlie a granitic basement and underlie a thick diabasic sill. The sedimentary section consists of Devonian sandstone and shale (Horlick formation), Carboniferous (?) tillite (Buckeye formation), Permian (?) platy and carbonaceous shale (Discovery Ridge formation), and Permian arkose, shale, and numerous coal beds (Mount Glossopteris formation). This apparently is the first report of a Paleozoic tillite in Antarctica. Article in Journal/Newspaper Antarc* Antarctica AAAS Resource Center (American Association for the Advancement of Science) Discovery Ridge ENVELOPE(-114.100,-114.100,-84.733,-84.733) Glossopteris ENVELOPE(-113.717,-113.717,-84.733,-84.733) Horlick Mountains ENVELOPE(-120.000,-120.000,-85.000,-85.000) Mount Glossopteris ENVELOPE(-113.717,-113.717,-84.733,-84.733) Science 136 3513 319 321 |
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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 |
In the Buckeye Range of the Horlick Mountains, 4000 feet of sedimentary rocks nonconformably overlie a granitic basement and underlie a thick diabasic sill. The sedimentary section consists of Devonian sandstone and shale (Horlick formation), Carboniferous (?) tillite (Buckeye formation), Permian (?) platy and carbonaceous shale (Discovery Ridge formation), and Permian arkose, shale, and numerous coal beds (Mount Glossopteris formation). This apparently is the first report of a Paleozoic tillite in Antarctica. |
format |
Article in Journal/Newspaper |
author |
Long, William E. |
spellingShingle |
Long, William E. Sedimentary Rocks of the Buckeye Range, Horlick Mountains, Antarctica |
author_facet |
Long, William E. |
author_sort |
Long, William E. |
title |
Sedimentary Rocks of the Buckeye Range, Horlick Mountains, Antarctica |
title_short |
Sedimentary Rocks of the Buckeye Range, Horlick Mountains, Antarctica |
title_full |
Sedimentary Rocks of the Buckeye Range, Horlick Mountains, Antarctica |
title_fullStr |
Sedimentary Rocks of the Buckeye Range, Horlick Mountains, Antarctica |
title_full_unstemmed |
Sedimentary Rocks of the Buckeye Range, Horlick Mountains, Antarctica |
title_sort |
sedimentary rocks of the buckeye range, horlick mountains, antarctica |
publisher |
American Association for the Advancement of Science (AAAS) |
publishDate |
1962 |
url |
http://dx.doi.org/10.1126/science.136.3513.319 https://www.science.org/doi/pdf/10.1126/science.136.3513.319 |
long_lat |
ENVELOPE(-114.100,-114.100,-84.733,-84.733) ENVELOPE(-113.717,-113.717,-84.733,-84.733) ENVELOPE(-120.000,-120.000,-85.000,-85.000) ENVELOPE(-113.717,-113.717,-84.733,-84.733) |
geographic |
Discovery Ridge Glossopteris Horlick Mountains Mount Glossopteris |
geographic_facet |
Discovery Ridge Glossopteris Horlick Mountains Mount Glossopteris |
genre |
Antarc* Antarctica |
genre_facet |
Antarc* Antarctica |
op_source |
Science volume 136, issue 3513, page 319-321 ISSN 0036-8075 1095-9203 |
op_doi |
https://doi.org/10.1126/science.136.3513.319 |
container_title |
Science |
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136 |
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3513 |
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319 |
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321 |
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1801380969058402304 |