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

Fisher, L A; Kendrick, Mark


The 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

CollectionsANU Research Publications
Date published: 2008
Type: Journal article
Source: Mineralium Deposita
DOI: 10.1007/s00126-008-0178-2


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