Study of a mafic layered intrusion of the Bathurst-Newcastle Area, N.B. (The River Complex)

dc.contributor.advisorMcAllister, A.
dc.contributor.authorBriand, Irene
dc.date.accessioned2023-06-07T22:02:39Z
dc.date.available2023-06-07T22:02:39Z
dc.date.issued1984
dc.description.abstractThis project is a study of a small mafic-ultramafic intrusion situated in Northumberland County, N.B. This body has been assigned an Early Devonian age and is intruded by granodiorite (also petrographically described) of a younger age. The gabbroic complex consists of what is proposed to be a differentiated- related rock series of peridotite, olivine gabbro and gabbro. A magmatic nickel-copper-iron sulphide assemglage is present. This appears to have crystallized from an immiscible sulphide liquid slightly after crystallization of the silicate•phases.
dc.description.copyrightNot available for use outside of the University of New Brunswick
dc.description.noteUniversity of New Brunswick. Department of Geology.
dc.format.extentiv, 52 pages
dc.identifier.urihttps://unbscholar.lib.unb.ca/handle/1882/36204
dc.language.isoen_CA
dc.publisherUniversity of New Brunswick
dc.rightshttp://purl.org/coar/access_right/c_16ec
dc.subject.disciplineEarth Sciences
dc.titleStudy of a mafic layered intrusion of the Bathurst-Newcastle Area, N.B. (The River Complex)
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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