A test of the viability of fluid-wall rock interaction mechanisms for changes in opaque phase assemblage in metasedimentary rocks in the Kambalda-St. Ives goldfield, Western Australia
Transitions from pyrrhotite-magnetite- to pyrite-magnetite- and pyrite-hematite-bearing assemblages in metasedimentary rocks in the Kambalda-St Ives goldfield have been shown to be spatially associated with economic gold grades. Fluid mixing, fluid-rock interaction and phase separation have been pr...
| Main Author: | |
|---|---|
| Format: | Journal Article |
| Published: |
Springer
2009
|
| Subjects: | |
| Online Access: | http://hdl.handle.net/20.500.11937/36597 |