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Southern provenance of upper Jackfork Sandstone, southern Ouachita Mountains: Cathodoluminescence petrology

1986; Geological Society of America; Volume: 97; Issue: 1 Linguagem: Inglês

10.1130/0016-7606(1986)97 2.0.co;2

1943-2674

Michael R. Owen, Albert V. Carozzi,

Geological Modeling and Analysis

Research Article| January 01, 1986 Southern provenance of upper Jackfork Sandstone, southern Ouachita Mountains: Cathodoluminescence petrology MICHAEL R. OWEN; MICHAEL R. OWEN 1Department of Geology, University of Illinois, 245 Natural History Building, 1301 W. Green St., Urbana, Illinois 61801 Search for other works by this author on: GSW Google Scholar ALBERT V. CAROZZI ALBERT V. CAROZZI 1Department of Geology, University of Illinois, 245 Natural History Building, 1301 W. Green St., Urbana, Illinois 61801 Search for other works by this author on: GSW Google Scholar Author and Article Information MICHAEL R. OWEN 1Department of Geology, University of Illinois, 245 Natural History Building, 1301 W. Green St., Urbana, Illinois 61801 ALBERT V. CAROZZI 1Department of Geology, University of Illinois, 245 Natural History Building, 1301 W. Green St., Urbana, Illinois 61801 Publisher: Geological Society of America First Online: 01 Jun 2017 Online ISSN: 1943-2674 Print ISSN: 0016-7606 Geological Society of America GSA Bulletin (1986) 97 (1): 110–115. https://doi.org/10.1130/0016-7606(1986)97 2.0.CO;2 Article history First Online: 01 Jun 2017 Cite View This Citation Add to Citation Manager Share Icon Share Facebook Twitter LinkedIn Email Permissions Search Site Citation MICHAEL R. OWEN, ALBERT V. CAROZZI; Southern provenance of upper Jackfork Sandstone, southern Ouachita Mountains: Cathodoluminescence petrology. GSA Bulletin 1986;; 97 (1): 110–115. doi: https://doi.org/10.1130/0016-7606(1986)97 2.0.CO;2 Download citation file: Ris (Zotero) Refmanager EasyBib Bookends Mendeley Papers EndNote RefWorks BibTex toolbar search Search Dropdown Menu toolbar search search input Search input auto suggest filter your search All ContentBy SocietyGSA Bulletin Search Advanced Search Abstract The source urea of the upper Jackfork Sandstone of the southern Ouachita Mountains of Arkansas has been located by means of Cathodoluminescence (CL) of quartz in conjunction with standard petrography. Comparison of frequency distributions of quartz CL colors between the Jackfork and approximately coeval sandstones of the Black Warrior basin detected genetically based affinities which were not apparent by inspection of gross petrology.The upper Jackfork was derived from the same source area as the Parkwood Formation of the Black Warrior basin of Alabama. The Parkwood is known to have come from the south, and so the Jackfork did also. The Jackfork represents a deep-water lithologic equivalent of the deltaic and nearshore marine Parkwood, deposited as turbidites in the deeper water of the Ouachita trough. First Page Preview Close Modal You do not have access to this content, please speak to your institutional administrator if you feel you should have access.