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Please use this identifier to cite or link to this item: https://superindex.lbr.auckland.ac.nz/handle/123456789/65347
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dc.creatorMcFadden, Rory-
dc.date.accessioned2013-05-31T01:53:27Z-
dc.date.available2013-05-31T01:53:27Z-
dc.date.issued2009-
dc.identifier.urihttp://hdl.handle.net/123456789/65347-
dc.description.abstractExpansive cliff-face exposures in the Fosdick Mountains (Antarctica) migmatite-cored gneiss dome enabled the documentation of suprasolidus deformation and melt migration structures in middle to lower crustal rocks at a scale significant for continental differentiation and crustal flow.-
dc.relation.urihttp://gradworks.umi.com/33/66/3366903.html-
dc.subjectCretaceous geology-
dc.titleMelt transport and magma accumulation in a migmatite cored gnesiss dome, Fosdick Mountains, West Antarctica-
thesis.degree.levelPhD-
thesis.degree.grantorUniversity of Minnesota (USA)-
dcterms.spatialFosdick Mountains Antarctica-
dcterms.spatialGondwana-
dcterms.spatialMarie Byrd Land-
dc.subject.keywordsmigmatite-
dc.subject.keywordsgnesiss-
Appears in Collections:Earth Science Theses

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