Petrography, alteration and deformation of the Toussaint Shear Zone, Verneuil, Quebec.

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dc.contributor.advisorBachinski, Don
dc.contributor.authorBliss, Ian C.
dc.date.accessioned2023-06-07T18:59:41Z
dc.date.available2023-06-07T18:59:41Z
dc.date.issued1995
dc.description.abstractThe principal gold mineralization on the GOG-CGK property in Verneuil, Quebec is completely hosted within the Toussaint Shear Zone (TZS). The shear zone is parallel to sub-parallel to lithologic units and has a sharp footwall contact with diorite and a more gradational contact with gabbro hanging wall. The majority of the shear zone is hosted within an intermediate volcanogenic/crystal tuff unit but also extends into the gabbro. The maximum width of the shear zone is 27 metres. Four mineralized horizons occur in the TZS of which two are sub-economic having values between 0.4 and 3 ppm Au. All of these horizons are parallel/sub-parallel to the lithological contacts. The two 'low gold horizons' outline the hanging- and footwall limits of the shear zone.
dc.description.copyrightNot available for use outside of the University of New Brunswick
dc.description.noteUniversity of New Brunswick. Department of Geology
dc.format.extentvii, 32 pages
dc.format.mediumelectronic
dc.identifier.urihttps://unbscholar.lib.unb.ca/handle/1882/32252
dc.language.isoen_CA
dc.publisherUniversity of New Brunswick
dc.rightshttp://purl.org/coar/access_right/c_16ec
dc.subject.disciplineEarth Sciences
dc.titlePetrography, alteration and deformation of the Toussaint Shear Zone, Verneuil, Quebec.
dc.typesenior report
thesis.degree.disciplineEarth Sciences
thesis.degree.fullnameBachelor of Science
thesis.degree.grantorUniversity of New Brunswick
thesis.degree.levelundergraduate
thesis.degree.nameB.Sc.

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