The Pacific Ocean formed through Neoproterozoic rifting of Rodinia and despite a long
history of plate convergence, this ocean has never subsequently closed. The record of …

The Tasmanides occupy the eastern third of Australia and provide an extensive record of the
evolution of the eastern Gondwanan convergent plate boundary from the Cambrian to the …

This paper presents a brief synthesis of the current state of knowledge on the formation and
break-up of the early-Neoproterozoic supercontinent Rodinia, and the subsequent assembly …

We present a full seismic waveform tomography for upper-mantle structure in the
Australasian region. Our method is based on spectral-element simulations of seismic wave …

Abstract The Tasmanides of eastern Australia record the break-up of Rodinia, followed by
the growth of orogenic belts along the eastern margin of Gondwana. Spatially, the …

The well-known southwest-to-northeast younging of stratigraphy over a present-day cross
strike distance of> 1500 km in the southern Tasmanides of eastern Australia has been used …

The Lachlan Orogen, like many other orogenic belts, has undergone paradigm shifts from
geosynclinal to plate-tectonic theory of evolution over the past 40 years. Initial plate-tectonic …

Sp and Ps scattered wave receiver functions were calculated for nineteen stations across
Australia and the island of Tasmania in order to image the lithosphere–asthenosphere …

In 2001 and 2002, a temporary array of 72 seismic recorders was deployed across northern
Tasmania (SE Australia), with the aim of imaging the underlying crust and upper mantle …

Australia boasts arguably the richest Late Neogene to Quaternary faulting record in stable
continental region (SCR) crust anywhere in the world. Variation in fault scarp length, vertical …