Document Detail


Geology of the Central Portion of the Queen Maud Range, Transantarctic Mountains.
MedLine Citation:
PMID:  17841973     Owner:  NLM     Status:  PubMed-not-MEDLINE    
Abstract/OtherAbstract:
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.
Authors:
F A Wade; V L Yeats; J R Everett; D W Greenlee; K E Laprade; J C Shenk
Related Documents :
647173 - An investigation of the role of 'hypnosis', hypnotic susceptibility and hypnotic induct...
25086983 - The effects of season and sex upon the morphology and material properties of keratin in...
16875823 - A normative sample of temporal and spatial gait parameters in children using the gaitri...
Publication Detail:
Type:  Journal Article    
Journal Detail:
Title:  Science (New York, N.Y.)     Volume:  150     ISSN:  0036-8075     ISO Abbreviation:  Science     Publication Date:  1965 Dec 
Date Detail:
Created Date:  2010-06-08     Completed Date:  2010-07-02     Revised Date:  -    
Medline Journal Info:
Nlm Unique ID:  0404511     Medline TA:  Science     Country:  United States    
Other Details:
Languages:  eng     Pagination:  1808-9     Citation Subset:  -    
Export Citation:
APA/MLA Format     Download EndNote     Download BibTex
MeSH Terms
Descriptor/Qualifier:

From MEDLINE®/PubMed®, a database of the U.S. National Library of Medicine


Previous Document:  Lead Isotopes and the Age of the Earth.
Next Document:  Migrant Sound Scatterers: Interaction with the Sea Floor.