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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Published in:Science
Main Author: Minshew, Velon H.
Format: Article in Journal/Newspaper
Language:English
Published: American Association for the Advancement of Science (AAAS) 1966
Subjects:
Online Access:http://dx.doi.org/10.1126/science.152.3722.637
https://www.science.org/doi/pdf/10.1126/science.152.3722.637
id craaas:10.1126/science.152.3722.637
record_format openpolar
spelling 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
institution 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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