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dc.contributor.advisorBorradaile, Graham J.
dc.contributor.authorDehls, John Fitzgerald
dc.date.accessioned2015-12-10T19:39:09Z
dc.date.available2015-12-10T19:39:09Z
dc.date.created1992
dc.date.issued1992
dc.identifier.urihttp://knowledgecommons.lakeheadu.ca/handle/2453/688
dc.description.abstractThe Seine Group metasedimentary rocks are situated between two converging major dextral transcurrent faults, the Quetico Fault to the north and the Seine River Fault to the south. To the west lies the Bad Vermillion Intrusive Complex (B.V.I.C.) The Seine Group shows one major period of metamorphism resulting in major F. folds. Regional metamorphism of chlorite to biotite zone greenschist facies was synkinematic with the deformation. Later minor deformations include localised crenulation cleavage and faults and shear zones.en_US
dc.language.isoen_USen_US
dc.subjectGeomagnetismen_US
dc.subjectGeologyen_US
dc.subjectMine Centre Regionen_US
dc.titleThe magnetic fabrics and strain history of the Achean Seine Group metasedimentary rocks near Mine Centre, Northwestern Ontarioen_US
etd.degree.nameM. Sc.en_US
etd.degree.levelMasteren_US
etd.degree.disciplineGeologyen_US
etd.degree.grantorLakehead Universityen_US


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