BEDDING GEOMETRY IN A PENNSYLVANIAN CHANNEL SANDSTONE

Research Article| July 01, 1967 BEDDING GEOMETRY IN A PENNSYLVANIAN CHANNEL SANDSTONE EDWARD C BEUTNER; EDWARD C BEUTNER DEPT. GEOLOGY AND GEOPHYSICS, THE PENNSYLVANIA STATE UNIVERSITY, UNIVERSITY PARK, PENNSYLVANIA Search for other works by this author on: GSW Google Scholar LINDA A FLUECKINGER; LINDA A FLUECKINGER DEPT. GEOLOGY AND GEOPHYSICS, THE PENNSYLVANIA STATE UNIVERSITY, UNIVERSITY PARK, PENNSYLVANIA Search for other works by this author on: GSW Google Scholar THEODORE M CARD THEODORE M CARD DEPT. GEOLOGY AND GEOPHYSICS, THE PENNSYLVANIA STATE UNIVERSITY, UNIVERSITY PARK, PENNSYLVANIA Search for other works by this author on: GSW Google Scholar Author and Article Information EDWARD C BEUTNER DEPT. GEOLOGY AND GEOPHYSICS, THE PENNSYLVANIA STATE UNIVERSITY, UNIVERSITY PARK, PENNSYLVANIA LINDA A FLUECKINGER DEPT. GEOLOGY AND GEOPHYSICS, THE PENNSYLVANIA STATE UNIVERSITY, UNIVERSITY PARK, PENNSYLVANIA THEODORE M CARD DEPT. GEOLOGY AND GEOPHYSICS, THE PENNSYLVANIA STATE UNIVERSITY, UNIVERSITY PARK, PENNSYLVANIA Publisher: Geological Society of America Received: 18 Apr 1966 First Online: 02 Mar 2017 Online ISSN: 1943-2674 Print ISSN: 0016-7606 Copyright © 1967, The Geological Society of America, Inc. Copyright is not claimed on any material prepared by U.S. government employees within the scope of their employment. GSA Bulletin (1967) 78 (7): 911–916. https://doi.org/10.1130/0016-7606(1967)78[911:BGIAPC]2.0.CO;2 Article history Received: 18 Apr 1966 First Online: 02 Mar 2017 Cite View This Citation Add to Citation Manager Share Icon Share Facebook Twitter LinkedIn Email Permissions Search Site Citation EDWARD C BEUTNER, LINDA A FLUECKINGER, THEODORE M CARD; BEDDING GEOMETRY IN A PENNSYLVANIAN CHANNEL SANDSTONE. GSA Bulletin 1967;; 78 (7): 911–916. doi: https://doi.org/10.1130/0016-7606(1967)78[911:BGIAPC]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 Cross-bedded sandstone in the Pennsylvanian Kittanning Formation of the Allegheny Group exposed in a strip mine near Philipsburg, Pennsylvania, consists of large, inclined, sigmoid sedimentation units that overlap each other uniformly toward the west. Such features as the arrangement of sedimentation units and their internal bedding geometry suggest that the sandstone originated by deposition on the inside of a meander curve of a westwardly migrating stream channel. 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.