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A Geochemical and Petrographical Study of Pillow Lavas from the Thetford Mines Ophiolite Complex, Quebec

dc.contributor.advisorShaw, D.M.
dc.contributor.authorMalczak, J.
dc.contributor.departmentGeologyen_US
dc.date.accessioned2025-01-23T03:08:12Z
dc.date.available2025-01-23T03:08:12Z
dc.date.issued1976-04
dc.description.abstractThe pillow lava samples analyzed from the Thetford Mines ophiolite complex have petrographical and geochemical characteristics similar to those of metamorphosed mid-oceanic basalts. The rocks have undergone submarine weathering and low grade metamorphism typical of the greenschist facies. The chemical analyses support the hypothesis that only part of pillow basalt unit of the ophiolite was altered sufficiently to produce a spilitic basalt.en_US
dc.description.degreeBachelor of Science (BSc)en_US
dc.description.degreetypeThesisen_US
dc.identifier.urihttp://hdl.handle.net/11375/30923
dc.language.isoenen_US
dc.subjectVolcanic rocken_US
dc.subjectPillow lavaen_US
dc.subjectThetford Mineen_US
dc.subjectMineralogyen_US
dc.subjectMetamorphismen_US
dc.titleA Geochemical and Petrographical Study of Pillow Lavas from the Thetford Mines Ophiolite Complex, Quebecen_US
dc.typeThesisen_US

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