P-T-t evolution of a large, long-lived, ultrahigh-temperature Grenvillian belt in central Australia
The ~120,000 km2 Musgrave Province forms part of a continuous Musgrave-Albany-Fraser mid-late Mesoproterozoic orogenic system that transects central and southern Australia, and continues into formerly contiguous Antarctica. Voluminous felsic magmatic rocks that intruded over the interval 1330-1150 M...
| Main Authors: | , , , , , , |
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| Format: | Journal Article |
| Published: |
Elsevier BV
2015
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| Online Access: | http://hdl.handle.net/20.500.11937/61634 |