Hayden, Travis G. et al. (2011): One dimensional backstripping results from IODP Expedition 318, Site U1356; tectonic implications for the Wilkes Land margin of Antarctica

Leg/Site/Hole:
IODP 318
IODP 318 U1356
Identifier:
2013-009998
georefid

Creator:
Hayden, Travis G.
Western Michigan University, Department of Geosciences, Kalamazoo, MI, United States
author

Kominz, Michelle A.
CSIC-Universidad de Granada, Spain
author

Gonzalez, Jhon
Utrecht University, Netherlands
author

Escutia Dotti, Carlota
author

Brinkhuis, Henk
author

Klaus, A.
author

Fehr, A.
author

Williams, T.
author

Bendle, J.
author

Bijl, Peter K.
author

Bohaty, S.
author

Carr, S.
author

Dunbar, R.
author

Iwai, M.
author

Jiminez-Espejo, F.
author

Katsuki, K.
author

Kong, G.
author

McKay, R.
author

Nakai, M.
author

Olney, M.
author

Passchier, S.
author

Pekar, S.
author

Sugisaki, S.
author

Tauxe, L.
author

Tuo, S.
author

van de Flierdt, C.
author

Welsh, K.
author

Yamane, M.
author

Pross, J.
author

Riesselman, C.
author

Roehl, U.
author

Sakai, T.
author

Shrivastava, P.
author

Stickley, C.
author

Identification:
One dimensional backstripping results from IODP Expedition 318, Site U1356; tectonic implications for the Wilkes Land margin of Antarctica
2011
In: Anonymous, Geological Society of America, 2011 annual meeting
Geological Society of America (GSA), Boulder, CO, United States
43
5
99-100
Wilkes Land is the conjugate margin of the Great Australian Bight, which underwent extension, thinning and rifting from approximately 160 Ma until breakup at approximately 83 Ma. Both Wilkes Land and the Great Australian Bight are considered passive margins, and were thought to be tectonically inactive since breakup at 83 Ma. We have backstripped the U1356 Core recovered from the continental rise off Wilkes Land, Antarctica by IODP Expedition 318. Backstripping input included lithological and sedimentary analysis, paleo-environmental indicators, combined paleomagnetic and biostratigraphic chronologies, and physical properties measurements. Tectonic subsidence shows a major event between 50 and 33.6 Ma, a time represented by a hiatus in the U1356 core. The magnitude of subsidence requires it to be tectonic in origin, and the timing matches with a reorganization of plate motions that represents the transition from slow spreading to fast spreading between Antarctica and Australia, which occurred at approximately 43 Ma. Coupled with a regional seismic framework, and using other Expedition 318 site analyses, the Wilkes Land margin is shown to be far more complex then the simple passive margin currently assumed. We explore several possible causes for the subsidence observed. One clue might be the tertiary episodic volcanism of Southeast Australia, which is suggested to be driven by lithospheric edge effect convection in the asthenosphere. Additional co-authors: A. Klaus, A. Fehr, T. Williams, J. Bendle, P. Bijl, S. Bohaty, S. Carr, R. Dunbar, M. Iwai, F. Jimenez-Espejo, K. Katsuki, G. Kong, R. McKay, M. Nakai, M. Olney, S. Passchier, S. Pekar, S. Sugisaki, L. Tauxe, S. Tuo, C. van de Flierdt, K. Welsh, M. Yamane, J. Pross, C. Riesselman, U. Rohl, T. Sakai, P. Shrivastava, C. Stickley, Expedition 318 Scientific Participants.
English
Coverage:Geographic coordinates:
North:-63.1837
West:135.5956East: 135.5956
South:-63.1837

Solid-earth geophysics; Antarctica; asthenosphere; Australasia; Australia; backstripping; biostratigraphy; continental rise; convection; cores; crustal thinning; Expedition 318; extension tectonics; geophysical methods; Great Australian Bight; Indian Ocean; Integrated Ocean Drilling Program; IODP Site U1356; measurement; ocean floors; one-dimensional models; passive margins; physical properties; plate tectonics; rifting; sea-floor spreading; seismic methods; southeastern Australia; Southern Ocean; tectonics; volcanism; Wilkes Land;

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