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Seafloor spreading / Continent-ocean boundary / Mid-ocean ridge / Rift / Oceanic crust / Non-volcanic passive margins / Passive margin / Geology / Plate tectonics / Continental crust


AUSTRALIAN-ANTARCTIC RIFTING Australian-Antarctic rifting J. M. Whittaker1, 3, R. D. Müller1 and A. Goncharov2 Keywords:
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Document Date: 2010-03-02 18:17:29


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City

Washington / DC / Canberra / College Station / Berlin / Leeds / Lang / Vienna / Cande / London / San Diego / Sydney / /

Company

WILSON / National Academies Press / Whittaker / /

Continent

Antarctica / /

Country

Austria / Australia / /

Facility

Scripps Institute of Oceanography / The University of Sydney / University of California / /

NaturalFeature

Southeast Indian Ocean / Great Australian Bight / Kerguelen Plateau / Normal sea / Eastern Indian Ocean / /

Organization

University of California / University of Sydney / Geological Society of London / EGU General Assembly / Geological Society / School of Geosciences / Scripps Institute of Oceanography / /

Person

VAN AVENDONK / /

Position

D. J. / polyphase evolution model of margin development / Major / /

ProvinceOrState

Texas / Sandwell / South Carolina / Newfoundland / California / /

PublishedMedium

Journal of Geophysical Research / /

Region

Antarctic / southern Australia / East Antarctica / east Antarctic / Southeast Indian Ocean / Eastern Indian Ocean / /

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