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

Date

Authors

Fisher, L A

Kendrick, Mark

Publisher

Springer Verlag

Abstract

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

Keywords

Keywords: 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

URI

http://hdl.handle.net/1885/65395

Collections

ANU Research Publications

Source

Mineralium Deposita

Type

Journal article

DOI

10.1007/s00126-008-0178-2

Restricted until

2037-12-31

Downloads

File

Description

01_Fisher_Metamorphic_fluid_origins_in_2008.pdf (738.7 KB)

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