Crustal architecture of the oblique-slip conjugate margins of George V Land and southeast Australia

A conceptual, lithospheric-scale cross-section of the conjugate, oblique-slip margins of George V Land, East
Antarctica, and southeast Australia (Otway Basin) has been constructed based on the integration of seismic and sample
data. This cross-section is characterised by asymmetry in width and thickness, and depth-dependent crustal extension at
breakup in the latest Maastrichtian. The broad Antarctic margin (~360 km apparent rift width) developed on thick
crust (~42 km) of the Antarctic craton, whereas the narrow Otway margin (~220 km) developed on the thinner crust
(~31 km) of the Ross–Delamerian Orogen. The shallow basement (velocities ~5.5 km.s-1) and the deep continental
crust (velocities >6.4 km.s-1) appear to be largely absent across the central rift, while the mid-crustal, probably granitic
layer (velocities ~6 km.s-1) is preserved. Comparison with published numerical models suggests that the shallow
basement and deep crust may have been removed by simple shear, whereas the mid-crust has been ductilely deformed.