Differentiation trends of the teschenite sill, in Dalhousie, New Brunswick

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dc.contributor.advisorS. Bachinski
dc.contributor.authorChiswell, Paul G.
dc.date.accessioned2023-06-07T21:22:18Z
dc.date.available2023-06-07T21:22:18Z
dc.date.issued1979
dc.description.abstractAn analcime-bearing olivine gabbro (teschenite) sill intrudes Lower Devonian sediments and calcalkaline volcanic rocks of the Dalhousie area, northern New Brunswick. Petrographic examination of the 27 thin sections and 9 whole-rock chemical analyses of samples of the sill indicate that the teschenite formed by two separate injections of magma each of which independently underwent differentiation after emplacement.
dc.description.copyrightNot available for use outside of the University of New Brunswick
dc.description.note4 unnumbered pages before page 1
dc.description.noteuniversity of New Brunswick. Department of Geology.
dc.format.extent52 pages
dc.format.mediumelectronic
dc.identifier.urihttps://unbscholar.lib.unb.ca/handle/1882/35651
dc.language.isoen_CA
dc.publisherUniversity of New Brunswick
dc.rightshttp://purl.org/coar/access_right/c_16ec
dc.subject.disciplineEarth Sciences
dc.titleDifferentiation trends of the teschenite sill, in Dalhousie, 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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