Revised potential field model of the Gilmore Fault Zone
The Gilmore Fault Zone (GFZ) marks a distinct geophysical contrast between metasediments of the Wagga Metamorphic Belt (high gravity and low magnetic intensity) and the Macquarie Arc and Silurian rift basins (low gravity and high magnetic intensity) in the Eastern Lachlan Orogen, Australia. This stu...
| Main Authors: | , , , , |
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| Format: | Journal Article |
| Published: |
CSIRO Publishing
2017
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| Online Access: | http://hdl.handle.net/20.500.11937/69870 |