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dc.contributor.authorFortner, Charles Howard
dc.date.accessioned2014-03-03T20:08:32Z
dc.date.available2014-03-03T20:08:32Z
dc.date.issued2002-05
dc.identifier.otherfortner_charles_h_200205_ms
dc.identifier.urihttp://purl.galileo.usg.edu/uga_etd/fortner_charles_h_200205_ms
dc.identifier.urihttp://hdl.handle.net/10724/20544
dc.description.abstractMetamorphic conditions were estimated for the Tallulah Falls Formation in the vicinity of Woodall Shoals on the Chattooga River on the Georgia–South Carolina border. Thermal peak metamorphic conditions of 700 o C, 6.25kbar, and 0.65<aH O <1.0 were estimated using a variety of geothermometers and geobarometers applied to amphibolite, amphibole-garnet-biotite gneiss, and sillimanite-biotite-gneiss. Results from this study confirm Barrovian metamorphism in the eastern Blue Ridge.
dc.publisheruga
dc.rightspublic
dc.subjectGeothermometry
dc.subjectgeobarometry
dc.subjectmetamorphic conditions
dc.subjectTallulah Falls Formation
dc.subjectWoodall Shoals
dc.subjectSouth Carolina
dc.subjectGeorgia
dc.subjecteastern Blue Ridge
dc.subjectsouthern Appalachians
dc.subjectChattooga River
dc.titleMetamorphism at Woodall Shoals in the eastern Blue Ridge, Georgia - South Carolina
dc.typeThesis
dc.description.degreeMS
dc.description.departmentGeology
dc.description.majorGeology
dc.description.advisorAlberto Patino-Douce
dc.description.committeeAlberto Patino-Douce
dc.description.committeeMichael Roden
dc.description.committeeSamuel Swanson


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