Skip navigation
Skip navigation

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


File Description SizeFormat Image
01_Fisher_Metamorphic_fluid_origins_in_2008.pdf738.7 kBAdobe PDF    Request a copy

Items in Open Research are protected by copyright, with all rights reserved, unless otherwise indicated.

Updated:  17 November 2022/ Responsible Officer:  University Librarian/ Page Contact:  Library Systems & Web Coordinator