Metamorphic petrology of the Bird Lake area, southeastern Manitoba

dc.contributor.authorButrenchuk, S. B.en_US
dc.date.accessioned2012-05-10T21:13:55Z
dc.date.available2012-05-10T21:13:55Z
dc.date.issued1970en_US
dc.degree.disciplineEarth Sciencesen_US
dc.degree.levelMaster of Science (M.Sc.)en_US
dc.description.abstractA total of 114 samples was collected from the Bird Lake and Cat Lake greenstone belts. Thin sections were made from 100 samples in order to determine mineral assemblages and textures. Chemical analyses were done on 25 samples to determine their bulk composition and its relationship to the mineralogy. Five facies of metamorphism have been interpreted to be present in this area: 1. Albite-epidote hornfels facies 2. Hornblende-hornfels facies 3. Greenschist facies 4. Almandine-amphibolite facies (a. with epidote) 5. Almandine-amphibolite facies (b. without epidote) Facies one and two are products of a first period of thermal metamorphism. A second period of metamorphism, dyamo-thermal type,produced facies three, four and five as well as a regional foliation that is parallel to the original bedding. A third period of metamorphism, dynamic type, produced a poorly developed secondary foliation and shears along which chlorite formed. A gradient of intensity of deformation exists in this area. Recrystallization was greatest in the east and quartz-mica schists were developed. In the west the foliation is not well developed and the rocks have retained many of their original sedimentary features.en_US
dc.format.extent66 leaves :en_US
dc.identifierocm72755797en_US
dc.identifier.urihttp://hdl.handle.net/1993/5590
dc.language.isoengen_US
dc.rightsopen accessen_US
dc.titleMetamorphic petrology of the Bird Lake area, southeastern Manitobaen_US
dc.typemaster thesisen_US
local.subject.manitobayesen_US
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