The Farquharson Cu-Ni Zone Northwest Miramichi Area New Brunswick

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dc.contributor.advisorMcAllister, A.
dc.contributor.authorThomas, Neil
dc.date.accessioned2023-06-07T17:32:28Z
dc.date.available2023-06-07T17:32:28Z
dc.date.issued1984
dc.description.abstractThe study area is a sulphide/oxide mineralized zone within the Devonian age Goodwin Lake Gabbro. The Farquharson Zone is the site of an extensive diamond drill program by numerous companies to establish the economic potential of a large geophysics anomaly. Copper and nickel occur as chalcopyrite and pentlandite respectively, throughout the zone in minor quantities. The sulphide phases with which these minerals are associated are magmatic in origin, stemming from the evolution of a Sulphur saturated silicate melt.
dc.description.copyrightNot available for use outside of the University of New Brunswick
dc.description.noteUniversity of New Brunswick. Department of Geology.
dc.format.extentviii, 89 pages
dc.format.mediumelectronic
dc.identifier.urihttps://unbscholar.lib.unb.ca/handle/1882/30390
dc.language.isoen_CA
dc.publisherUniversity of New Brunswick
dc.rightshttp://purl.org/coar/access_right/c_16ec
dc.subject.disciplineEarth Sciences
dc.titleThe Farquharson Cu-Ni Zone Northwest Miramichi Area New Brunswick
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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