Abstract
Research Article| March 01, 1966 K-Ar AGES OF DETRITAL MUSCOVITE IN THE MERIDIAN SAND OF ALABAMA AND MISSISSIPPI E. G WERMUND; E. G WERMUND FIELD RESEARCH LABORATORY, SOCONY MOBIL OIL COMPANY, INC., DALLAS, TEXAS Search for other works by this author on: GSW Google Scholar W. H BURKE, JR.; W. H BURKE, JR. FIELD RESEARCH LABORATORY, SOCONY MOBIL OIL COMPANY, INC., DALLAS, TEXAS Search for other works by this author on: GSW Google Scholar G. S KENNY G. S KENNY FIELD RESEARCH LABORATORY, SOCONY MOBIL OIL COMPANY, INC., DALLAS, TEXAS Search for other works by this author on: GSW Google Scholar GSA Bulletin (1966) 77 (3): 319–322. https://doi.org/10.1130/0016-7606(1966)77[319:KAODMI]2.0.CO;2 Article history received: 15 Nov 1965 first online: 02 Mar 2017 Cite View This Citation Add to Citation Manager Share Icon Share Facebook Twitter LinkedIn MailTo Tools Icon Tools Get Permissions Search Site Citation E. G WERMUND, W. H BURKE, G. S KENNY; K-Ar AGES OF DETRITAL MUSCOVITE IN THE MERIDIAN SAND OF ALABAMA AND MISSISSIPPI. GSA Bulletin 1966;; 77 (3): 319–322. doi: https://doi.org/10.1130/0016-7606(1966)77[319:KAODMI]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 Eocene Meridian Sand of Mississippi and Alabama contains abundant large subhedral to anhedral flakes of muscovite (2M). K-Ar age determinations of the muscovite yield ages of 290 ± 6 and 308 ± 6 million years. The Meridian muscovite is detrital and was probably derived from the Appalachian Mountains to the east. This content is PDF only. Please click on the PDF icon to access. 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.
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