Metamorphic fluid origins in the Osborne Fe oxide - Cu - Au deposit, Australia: Evidence from noble gases and halogens
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Description
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 |
|---|---|
| Date published: | 2008 |
| Type: | Journal article |
| URI: | http://hdl.handle.net/1885/65395 |
| Source: | Mineralium Deposita |
| DOI: | 10.1007/s00126-008-0178-2 |
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| File | Description | Size | Format | Image |
|---|---|---|---|---|
| 01_Fisher_Metamorphic_fluid_origins_in_2008.pdf | 738.7 kB | Adobe PDF | Request a copy |
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