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Carboniferous microfacies, microfossils, and corals, Lisburne Group, Arctic Alaska / by Augustus K. Armstrong and Bernard L. Mamet.

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Format:
Book
Government document
Author/Creator:
Armstrong, Augustus K., author.
Mamet, Bernard L., author.
Contributor:
Geological Survey (U.S.), issuing body.
Series:
Geological Survey professional paper ; 849.
Geological Survey professional paper ; 849
Language:
English
Subjects (All):
Algae, Fossil.
Corals, Fossil.
Foraminifera, Fossil.
Geology--Alaska--Brooks Range.
Geology.
Geology, Stratigraphic--Carboniferous.
Geology, Stratigraphic.
geology.
Carboniferous Geologic Period.
Alaska--Brooks Range.
Medical Subjects:
Geology.
Genre:
Online resources.
Physical Description:
1 online resource (viii, 144 pages, 39 unnumbered pages of plates) : illustrations, maps.
Distribution:
Washington : United States Government Printing Office
Place of Publication:
Washington : United States Department of the Interior, Geological Survey, 1977.
Summary:
Description of Carboniferous foraminifers and algae with biostratigraphic zonation, relationship to carbonate facies, comparison with coral distribution, and correlations among northern Alaska, western Europe, and the midcontinent region of North America. One hundred species, of which 2 are new, and 61 genera are described and illustrated.
Notes:
Title from title screen (viewed October 6, 2014).
Also available online in PDF format from the U.S. Geological Survey Warehouse (http://pubs.er.usgs.gov/).
"Description of Carboniferous formaminifers and algae with biostratigraphic zonation, relationship to carbonate facies, comparison with coral distribution, and correlations among northern Alaska, western Europe, and the midcontinent region of North America. One hundred species, of which 2 are new, and 61 genera are described and illustrated."
Includes bibliographical references (pages 116-129) and index.
Other Format:
Print version: Armstrong, Augustus K. Carboniferous microfacies, microfossils, and corals, Lisburne Group, Arctic Alaska
OCLC:
896810453

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