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Neoarchean (2.7 Ga) reworking of the Ungava craton by Fe-rich parental magmas

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Identiferoai:union.ndltd.org:mcgill.ca/oai:escholarship.mcgill.ca:vq27zr74n
Date January 2014
CreatorsMilidragovic, Dejan
ContributorsDonald M Francis (Supervisor)
PublisherMcGill University
Source SetsMcGill University
Languagehttp://id.loc.gov/vocabulary/iso639-2/eng
Detected LanguageEnglish
TypeThesis
RightsAll items in eScholarship@McGill are protected by copyright with all rights reserved unless otherwise indicated.
RelationPid: 123146

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