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Metamorphic fluid origins in the Osborne Fe oxide - Cu - Au deposit, Australia: Evidence from noble gases and halogens

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dc.contributor.authorFisher, L A
dc.contributor.authorKendrick, Mark
dc.date.accessioned2015-12-10T23:17:54Z
dc.date.issued2008
dc.date.updated2015-12-10T10:02:22Z
dc.description.abstractThe Osborne iron oxide-copper-gold (IOCG) deposit is hosted by amphibolite facies metasedimentary rocks and associated with pegmatite sheets formed by anatexis during peak metamorphism. Eleven samples of ore-related hydrothermal quartz and two pegmatitic
dc.identifier.issn0026-4598
dc.identifier.urihttp://hdl.handle.net/1885/65395
dc.publisherSpringer Verlag
dc.sourceMineralium Deposita
dc.subjectKeywords: amphibolite; argon isotope; copper; dissolution; evaporite; fluid inclusion; gold; halogen; host rock; iron oxide; metasedimentary rock; mineralization; noble gas; ore deposit; Australasia; Australia; Mount Isa; Queensland Argon isotopes; Australia; Halogens; IOCG; Mt Isa; Osborne
dc.titleMetamorphic fluid origins in the Osborne Fe oxide - Cu - Au deposit, Australia: Evidence from noble gases and halogens
dc.typeJournal article
local.bibliographicCitation.issue5
local.bibliographicCitation.lastpage497
local.bibliographicCitation.startpage483
local.contributor.affiliationFisher, L A, James Cook University
local.contributor.affiliationKendrick, Mark, College of Physical and Mathematical Sciences, ANU
local.contributor.authoruidKendrick, Mark, u4746994
local.description.embargo2037-12-31
local.description.notesImported from ARIES
local.identifier.absfor040203 - Isotope Geochemistry
local.identifier.absseo970104 - Expanding Knowledge in the Earth Sciences
local.identifier.ariespublicationU3488905xPUB1099
local.identifier.citationvolume43
local.identifier.doi10.1007/s00126-008-0178-2
local.identifier.scopusID2-s2.0-47349115757
local.type.statusPublished Version

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