Stratigraphy of the Wisconsin Range, Horlick Mountains, Antarctica
The Wisconsin Range consists of a basement complex of granitic and metamorphic rocks unconformably overlain by about 550 meters of Upper Paleozoic sedimentary rocks. The base of the Upper Paleozoic succession is composed of the Buckeye formation, a tillite, which varies in thickness from 80 to more...
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American Association for the Advancement of Science (AAAS)
1966
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craaas:10.1126/science.152.3722.637 2024-06-09T07:39:06+00:00 Stratigraphy of the Wisconsin Range, Horlick Mountains, Antarctica Minshew, Velon H. 1966 http://dx.doi.org/10.1126/science.152.3722.637 https://www.science.org/doi/pdf/10.1126/science.152.3722.637 en eng American Association for the Advancement of Science (AAAS) Science volume 152, issue 3722, page 637-638 ISSN 0036-8075 1095-9203 journal-article 1966 craaas https://doi.org/10.1126/science.152.3722.637 2024-05-16T12:55:29Z The Wisconsin Range consists of a basement complex of granitic and metamorphic rocks unconformably overlain by about 550 meters of Upper Paleozoic sedimentary rocks. The base of the Upper Paleozoic succession is composed of the Buckeye formation, a tillite, which varies in thickness from 80 to more than 140 meters. Overlying the Buckeye formation are the Weaver and Queen Maud formations, with a combined thickness of about 455 meters, characterized by a prolific Glossopteris flora, indicative of a Permian age. Article in Journal/Newspaper Antarc* Antarctica AAAS Resource Center (American Association for the Advancement of Science) Weaver ENVELOPE(-153.833,-153.833,-86.967,-86.967) Glossopteris ENVELOPE(-113.717,-113.717,-84.733,-84.733) Horlick Mountains ENVELOPE(-120.000,-120.000,-85.000,-85.000) Wisconsin Range ENVELOPE(-125.000,-125.000,-85.500,-85.500) Science 152 3722 637 638 |
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Open Polar |
collection |
AAAS Resource Center (American Association for the Advancement of Science) |
op_collection_id |
craaas |
language |
English |
description |
The Wisconsin Range consists of a basement complex of granitic and metamorphic rocks unconformably overlain by about 550 meters of Upper Paleozoic sedimentary rocks. The base of the Upper Paleozoic succession is composed of the Buckeye formation, a tillite, which varies in thickness from 80 to more than 140 meters. Overlying the Buckeye formation are the Weaver and Queen Maud formations, with a combined thickness of about 455 meters, characterized by a prolific Glossopteris flora, indicative of a Permian age. |
format |
Article in Journal/Newspaper |
author |
Minshew, Velon H. |
spellingShingle |
Minshew, Velon H. Stratigraphy of the Wisconsin Range, Horlick Mountains, Antarctica |
author_facet |
Minshew, Velon H. |
author_sort |
Minshew, Velon H. |
title |
Stratigraphy of the Wisconsin Range, Horlick Mountains, Antarctica |
title_short |
Stratigraphy of the Wisconsin Range, Horlick Mountains, Antarctica |
title_full |
Stratigraphy of the Wisconsin Range, Horlick Mountains, Antarctica |
title_fullStr |
Stratigraphy of the Wisconsin Range, Horlick Mountains, Antarctica |
title_full_unstemmed |
Stratigraphy of the Wisconsin Range, Horlick Mountains, Antarctica |
title_sort |
stratigraphy of the wisconsin range, horlick mountains, antarctica |
publisher |
American Association for the Advancement of Science (AAAS) |
publishDate |
1966 |
url |
http://dx.doi.org/10.1126/science.152.3722.637 https://www.science.org/doi/pdf/10.1126/science.152.3722.637 |
long_lat |
ENVELOPE(-153.833,-153.833,-86.967,-86.967) ENVELOPE(-113.717,-113.717,-84.733,-84.733) ENVELOPE(-120.000,-120.000,-85.000,-85.000) ENVELOPE(-125.000,-125.000,-85.500,-85.500) |
geographic |
Weaver Glossopteris Horlick Mountains Wisconsin Range |
geographic_facet |
Weaver Glossopteris Horlick Mountains Wisconsin Range |
genre |
Antarc* Antarctica |
genre_facet |
Antarc* Antarctica |
op_source |
Science volume 152, issue 3722, page 637-638 ISSN 0036-8075 1095-9203 |
op_doi |
https://doi.org/10.1126/science.152.3722.637 |
container_title |
Science |
container_volume |
152 |
container_issue |
3722 |
container_start_page |
637 |
op_container_end_page |
638 |
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1801377240898863104 |