Metamorphic fluid origins in the Osborne Fe oxide - Cu - Au deposit, Australia: Evidence from noble gases and halogens
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
|Collections||ANU Research Publications|
|01_Fisher_Metamorphic_fluid_origins_in_2008.pdf||738.7 kB||Adobe PDF||Request a copy|
Items in Open Research are protected by copyright, with all rights reserved, unless otherwise indicated.