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Origin and Metamorphism of Part of the Hermon Group Near Bancroft, Ontario

dc.contributor.advisorShaw, Denis M.
dc.contributor.authorJennings, David S.
dc.contributor.departmentGeologyen_US
dc.date.accessioned2016-07-18T21:05:12Z
dc.date.available2016-07-18T21:05:12Z
dc.date.issued1969-11
dc.descriptionTitle: Origin and Metamorphism of Part of the Hermon Group Near Bancroft, Ontario, Author: David S. Jennings, Location: Thodeen_US
dc.description.abstract<p>A detailed geological and petrochernical study of an upper amphibolite grade, "Grenville Series" sequence is presented. Integrated structural, stratigraphic and geochemical data have led to the conclusion that this seqluence accumulated as an interbanded volcanic and sedimentary prism either in an Upper Proterozoic geosyncline or volcano-tectonic depression .</p> <p>Metamorphic phase assemblages, in general, approach equilibrium. As assemblage showing disequilibrium, "frozen", re - actions are discussed in detail. Experimental data on all the phase assemblages suggests the most probable range of metamorphic conditions to be 625° to 690° and 5. 5 to 7 kilobars total pressure. The 11 effects of retrograde metamorphism on the prograde assemblages are documented.</p>en_US
dc.description.degreeDoctor of Philosophy (PhD)en_US
dc.description.degreetypeThesisen_US
dc.identifier.urihttp://hdl.handle.net/11375/19836
dc.language.isoenen_US
dc.titleOrigin and Metamorphism of Part of the Hermon Group Near Bancroft, Ontarioen_US
dc.typeThesisen_US

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