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Tectonic geomorphology of Australia
2010
Geological Society Special Publication
The Australian continent is actively deforming in response to far-field stresses generated by plate boundary interactions and buoyancy forces associated with mantle dynamics. On the largest scale (several 10 3 km), the submergence of the northern continental shelf is driven by dynamic topography caused by mantle downwelling along the Indo-Pacific subduction system and accentuated by a regionally elevated geoid. The emergence of the southern shelf is attributed to the progressive movement of
doi:10.1144/sp346.13
fatcat:kmqxogmycbhind3zngm4pfi7ym