Unraveling the New England orocline, east Gondwana accretionary margin
The New England orocline lies within the Eastern Australian segment of the Terra Australis accretionary orogen and developed during the late Paleozoic to early Mesozoic Gondwanide Orogeny (310–230 Ma) that extended along the Pacific margin of the Gondwana supercontinent. The orocline deformed a pre-...
| Main Authors: | , , |
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| Format: | Journal Article |
| Published: |
American Geophysical Union
2011
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| Subjects: | |
| Online Access: | http://hdl.handle.net/20.500.11937/14959 |