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Lower Llandovery of the Northern Appalachians and Adjacent Regions
17
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1969
Year
EngineeringGeomorphologyEarth ScienceRegional GeologySocial SciencesNatural ResourcesQuaternary ResearchGeological DataLower LlandoveryNorthern AppalachiansGeographyGeologySedimentologyAdjacent RegionsExploration GeologyEconomic GeologyEarth SciencesGeochemistryPaleoecologyQuaternary PeriodMountain Uplift
Research Article| March 01, 1969 Lower Llandovery of the Northern Appalachians and Adjacent Regions WILLIAM G AYRTON; WILLIAM G AYRTON Pan American Petroleum Corporation, Calgary, Alberta 1 Alphabetical listing of authors. Search for other works by this author on: GSW Google Scholar WILLIAM B. N BERRY; WILLIAM B. N BERRY University of California, Berkeley, California 94720 Search for other works by this author on: GSW Google Scholar ARTHUR J BOUCOT; ARTHUR J BOUCOT University of Pennsylvania, Philadelphia, Pennsylvania 19104 Search for other works by this author on: GSW Google Scholar JEAN LAJOIE; JEAN LAJOIE Universite de Montreal, Montreal, Quebec Search for other works by this author on: GSW Google Scholar PIERRE J LESPERANCE; PIERRE J LESPERANCE Universite de Montreal, Montreal, Quebec Search for other works by this author on: GSW Google Scholar LOUIS PAVLIDES; LOUIS PAVLIDES U.S. Geological Survey, Washington, D. C. 20242 Search for other works by this author on: GSW Google Scholar W. BRIAN SKIDMORE W. BRIAN SKIDMORE Department of Natural Resources, Quebec, Quebec Search for other works by this author on: GSW Google Scholar Author and Article Information WILLIAM G AYRTON 1 Alphabetical listing of authors. Pan American Petroleum Corporation, Calgary, Alberta WILLIAM B. N BERRY University of California, Berkeley, California 94720 ARTHUR J BOUCOT University of Pennsylvania, Philadelphia, Pennsylvania 19104 JEAN LAJOIE Universite de Montreal, Montreal, Quebec PIERRE J LESPERANCE Universite de Montreal, Montreal, Quebec LOUIS PAVLIDES U.S. Geological Survey, Washington, D. C. 20242 W. BRIAN SKIDMORE Department of Natural Resources, Quebec, Quebec Publisher: Geological Society of America Received: 18 Mar 1968 Revision Received: 23 Aug 1968 First Online: 02 Mar 2017 Online ISSN: 1943-2674 Print ISSN: 0016-7606 Copyright © 1969, 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 (1969) 80 (3): 459–484. https://doi.org/10.1130/0016-7606(1969)80[459:LLOTNA]2.0.CO;2 Article history Received: 18 Mar 1968 Revision Received: 23 Aug 1968 First Online: 02 Mar 2017 Cite View This Citation Add to Citation Manager Share Icon Share Facebook Twitter LinkedIn Email Permissions Search Site Citation WILLIAM G AYRTON, WILLIAM B. N BERRY, ARTHUR J BOUCOT, JEAN LAJOIE, PIERRE J LESPERANCE, LOUIS PAVLIDES, W. BRIAN SKIDMORE; Lower Llandovery of the Northern Appalachians and Adjacent Regions. GSA Bulletin 1969;; 80 (3): 459–484. doi: https://doi.org/10.1130/0016-7606(1969)80[459:LLOTNA]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 Rocks of clearly dated early Llandovery age, as well as rocks that can logically be classed as early Llandovery from their regional relationships, appear to be more widespread than recognized, heretofore, in the northern Appalachians and adjacent regions. Their areal distribution and lithology permit a generalized reconstruction of the paleogeography, which consisted, in general, of three source areas alternating from east to west with three belts of clastic sedimentation. The westernmost clastic belt grades laterally westward into the carbonate rocks of the North American platform. The Central Clastic Belt encloses a belt containing impure carbonates with clastic detritus and clastic interbeds, and, locally, relatively clean carbonate deposits.Llandovery age rocks of the platform include the Manitoulin Dolomite and the Ellis Bay Formation. In the deposits to the east, coeval rocks occur, in part or in whole, within the limy and clastic deposits of the Carys Mills Formation and the Matapedia Group, as well as in the following clastic rock formations: Grimsby, Shawangunk, Tuscarora, Massanutten, Clinch, Smyrna Mills, Perham, Cabano, Weir, Beechhill Cove, Ross Brook, and White Rock. 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.