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- W2034632597 abstract "Research Article| July 01, 1987 Brevard fault zone, southern Appalachians: A medium-angle, dextral, Alleghanian shear zone Alain Vauchez Alain Vauchez 1Laboratoire de Géologic dynamique et Pétrologie de la Surface et Unité Associée Centre National de la Recherche scientifique, Faculté des Sciences de St-Jérôme, 13397 Marseille, Cedex 13, France Search for other works by this author on: GSW Google Scholar Author and Article Information Alain Vauchez 1Laboratoire de Géologic dynamique et Pétrologie de la Surface et Unité Associée Centre National de la Recherche scientifique, Faculté des Sciences de St-Jérôme, 13397 Marseille, Cedex 13, France Publisher: Geological Society of America First Online: 02 Jun 2017 Online ISSN: 1943-2682 Print ISSN: 0091-7613 Geological Society of America Geology (1987) 15 (7): 669–672. https://doi.org/10.1130/0091-7613(1987)15<669:BFZSAA>2.0.CO;2 Article history First Online: 02 Jun 2017 Cite View This Citation Add to Citation Manager Share Icon Share Facebook Twitter LinkedIn MailTo Tools Icon Tools Get Permissions Search Site Citation Alain Vauchez; Brevard fault zone, southern Appalachians: A medium-angle, dextral, Alleghanian shear zone. Geology 1987;; 15 (7): 669–672. doi: https://doi.org/10.1130/0091-7613(1987)15<669:BFZSAA>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 SocietyGeology Search Advanced Search Abstract The record of Alleghanian movements in the rocks of the Brevard fault zone has been studied by using modern techniques of kinematic analysis. Mylonitic and phyllonitic fabric involves (1) strong subhorizontal stretching lineation trending northeast-southwest, parallel to the fault; (2) mylonitic foliation dipping moderately to the southeast; and (3) a great variety of kinematic indicators suggesting a dextral sense of shear. Both Palmetto and Ben Hill granites, Georgia (ca. 325 Ma), were sheared during this event, the age of which should be younger, probably ca. 310 Ma.The Brevard zone is usually regarded as a listric thrust fault along which the Piedmont terrains have been displaced toward the northwest onto the Blue Ridge. By contrast, the movement picture resulting from our analysis is compatible only with right-lateral strike-slip faulting along a moderately dipping shear zone several kilometres wide, causing southwestward displacement of the Piedmont relative to the Blue Ridge province, parallel to the Appalachian trend. 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." @default.
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- W2034632597 title "Brevard fault zone, southern Appalachians: A medium-angle, dextral, Alleghanian shear zone" @default.
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