Fe isotopes and the contrasting petrogenesis of A-, I- and S-type granite

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dc.contributor.authorFoden, J.
dc.contributor.authorSossi, P.
dc.contributor.authorWawryk, C.
dc.date.issued2015
dc.description.abstractAbstract not available
dc.description.statementofresponsibilityJohn Foden, Paolo A. Sossi, Christine M. Wawryk
dc.identifier.citationLithos, 2015; 212-215:32-44
dc.identifier.doi10.1016/j.lithos.2014.10.015
dc.identifier.issn0024-4937
dc.identifier.issn1872-6143
dc.identifier.orcidFoden, J. [0000-0003-3564-7253]
dc.identifier.urihttp://hdl.handle.net/2440/100406
dc.language.isoen
dc.publisherElsevier
dc.relation.granthttp://purl.org/au-research/grants/arc/DP110104686
dc.rights© 2014 Elsevier B.V. All rights reserved.
dc.source.urihttps://doi.org/10.1016/j.lithos.2014.10.015
dc.subjectGranite; iron isotopes; A-type granite; oxygen fugacity; buffering
dc.titleFe isotopes and the contrasting petrogenesis of A-, I- and S-type granite
dc.typeJournal article
pubs.publication-statusPublished

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