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Please use this identifier to cite or link to this item: http://hdl.handle.net/11375/19590
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dc.contributor.advisorCrocket, James H.-
dc.contributor.authorMcDonald, Dean W. A.-
dc.date.accessioned2016-06-20T22:31:38Z-
dc.date.available2016-06-20T22:31:38Z-
dc.date.issued1981-04-
dc.identifier.urihttp://hdl.handle.net/11375/19590-
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.titlePetrology and Geochemistry of Knobby Peridotite Zones within Unltramafic Flows at Pyke's Hill, Munro Township, Ontarioen_US
dc.typeThesisen_US
dc.contributor.departmentGeologyen_US
dc.description.degreetypeThesisen_US
dc.description.degreeBachelor of Science (BSc)en_US
Appears in Collections:Bachelor theses

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Title: Petrology and Geochemistry of Knobby Peridotite Zones within Unltramafic Flows at Pyke's Hill, Munro Township, Ontario, Author: Dean W. A. McDonald, Location: Thode7.06 MBAdobe PDFView/Open
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