| Geology of the Central Portion of the Queen Maud Range, Transantarctic Mountains. | |
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MedLine Citation:
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PMID: 17841973 Owner: NLM Status: PubMed-not-MEDLINE |
Abstract/OtherAbstract:
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The geologic section consists of a folded and metamorphosed basement complex of geosynclinal and nearshore sediments and intrusives, a thick sequence of nearshore and terrestrial sediments of middle to late Paleozoic age, and thick diabase sheets and basalt flows of Jurassic age. Block faulting, probably through during the Miocene age, produced the which has been carved into its present from by glaciers. |
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Authors:
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F A Wade; V L Yeats; J R Everett; D W Greenlee; K E Laprade; J C Shenk |
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Publication Detail:
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Type: Journal Article |
Journal Detail:
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Title: Science (New York, N.Y.) Volume: 150 ISSN: 0036-8075 ISO Abbreviation: Science Publication Date: 1965 Dec |
Date Detail:
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Created Date: 2010-06-08 Completed Date: 2010-07-02 Revised Date: - |
Medline Journal Info:
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Nlm Unique ID: 0404511 Medline TA: Science Country: United States |
Other Details:
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Languages: eng Pagination: 1808-9 Citation Subset: - |
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From MEDLINE®/PubMed®, a database of the U.S. National Library of Medicine
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