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Petrology and Geochemistry of Knobby Peridotite Zones within Unltramafic Flows at Pyke's Hill, Munro Township, Ontario

dc.contributor.advisorCrocket, James H.
dc.contributor.authorMcDonald, Dean W. A.
dc.contributor.departmentGeologyen_US
dc.date.accessioned2016-06-20T22:31:38Z
dc.date.available2016-06-20T22:31:38Z
dc.date.issued1981-04
dc.descriptionTitle: Petrology and Geochemistry of Knobby Peridotite Zones within Unltramafic Flows at Pyke's Hill, Munro Township, Ontario, Author: Dean W. A. McDonald, Location: Thodeen_US
dc.description.abstract<p>Knobby peridotite forms a distinctive zone within the cumulus member of spinifex and non-spinifex bearing ultramafic komatiitic flows. Detailed measurements of flows at Pyke's Hill indicate the relative abundance and spatial relationships of knobby peridotites within specific types of flows. Petrographic and geochemical analysis (including whole rock, rare earth and neutron activation) have been implemented and discussed in terms of a comparison to analysis of other zones within the flow. Polished sections indicate relationships between silicate and opaque mineralogy.</p>en_US
dc.description.degreeBachelor of Science (BSc)en_US
dc.description.degreetypeThesisen_US
dc.identifier.urihttp://hdl.handle.net/11375/19590
dc.titlePetrology and Geochemistry of Knobby Peridotite Zones within Unltramafic Flows at Pyke's Hill, Munro Township, Ontarioen_US
dc.typeThesisen_US

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