Unraveling the New England orocline, east Gondwana accretionary margin

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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-...

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Bibliographic Details
Main Authors:	Cawood, P., Pisarevsky, Sergei, Leitch, E.
Format:	Journal Article
Published:	American Geophysical Union 2011
Subjects:	magmatic activity coupling orocline formation Gondwana convergence
Online Access:	http://hdl.handle.net/20.500.11937/14959

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