The evolution of mafic and ultramafic rocks of the Mesoproterozoic Fraser Zone, Albany-Fraser Orogen, and implications for the Ni-Cu sulphide potential of the region
The Albany–Fraser Orogen is located along the southern and southeastern margins of the Archean Yilgarn Craton and formed from at least c. 1810 to 1140 Ma during reworking of the craton, accompanied by variable additions of juvenile mantle material. The Fraser Zone is an approximately 425 km long and...
| Main Authors: | , , , , , , |
|---|---|
| Format: | Report |
| Published: |
2016
|
| Online Access: | http://hdl.handle.net/20.500.11937/55374 |