HR: 0800h
AN: T41A-0377    [Abstracts]
TI: Rift tectonics in the Amundsen Sea Embayment: Stepwise break-up of New Zealand from West Antarctica
AU: * Gohl, K
EM: karsten.gohl@awi.de
AF: Alfred Wegener Institute for Polar and Marine Research, Columbusstrasse, Bremerhaven, 27568, Germany
AU: Eagles, G
EM: g.eagles@gl.rhul.ac.uk
AF: Alfred Wegener Institute for Polar and Marine Research, Columbusstrasse, Bremerhaven, 27568, Germany
AU: Grobys, J
EM: jangrobys@bwb.org
AF: Alfred Wegener Institute for Polar and Marine Research, Columbusstrasse, Bremerhaven, 27568, Germany
AU: Larter, R
EM: r.larter@bas.ac.uk
AF: British Antarctic Survey, High Cross, Madingley Road, Cambridge, CB3 0ET, United Kingdom
AU: Netzeband, G
EM: gnetzeband@ifm-geomar.de
AF: Institute of Geophysics, University of Hamburg, Bundesstr. 55, Hamburg, 20146, Germany
AU: Parsiegla, N
EM: nicole.parsiegla@awi.de
AF: Alfred Wegener Institute for Polar and Marine Research, Columbusstrasse, Bremerhaven, 27568, Germany
AU: Teterin, D
EM: d_e_teterin@mail.ru
AF: Vernadsky Institute of Geochemistry and Analytical Chemistry, 19 Kosygin St., Moscow, 117975, Russian Federation
AB: The Amundsen Sea Embayment of West Antarctica is in a prominent location for a series of tectonic and magmatic events from Paleozoic to Cenozoic times. It played a central role in the rifting and break-up of greater New Zealand from West Antarctica as it is the location where the junction of Chatham Rise and Campbell Plateau (New Zealand) lies conjugate to the West Antarctic margin. New seismic, magnetic and gravity data from the Amundsen Sea Embayment and Pine Island Bay reveal the crustal thickness and tectonic lineations. The Moho is 24-22 km deep on the shelf. NE-SW trending magnetic and gravity anomalies and the thin crust indicate a former rift zone that was active during or in the run-up to breakup between Chatham Rise and West Antarctica before or at 90 Ma. NW-SE trending gravity and magnetic anomalies, following a prolongation of Peacock Sound between Thurston Island and Ellsworth Land, indicate the extensional southern boundary to the Bellingshausen Plate which was active between 79 and 61 Ma. However, both lineation trends, NE-SW and NW-SE, seem to be observed over broad regions. This infers stepwise and multiple rift and extension phases over a wide period of time before, during and after the break-up between New Zealand and West Antarctica.
DE: 1209 Tectonic deformation (6924)
DE: 3025 Marine seismics (0935, 7294)
DE: 3040 Plate tectonics (8150, 8155, 8157, 8158)
DE: 3045 Seafloor morphology, geology, and geophysics
DE: 8105 Continental margins: divergent (1212, 8124)
SC: Tectonophysics [T]
MN: 2007 Fall Meeting