The New Guinea region evolved within the obliquely and rapidly converging Australian and
Pacific plate boundary zone. It is arguably one of the most tectonically complex regions of …

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 …

Weathering intensity largely controls the degree to which primary minerals are altered to
secondary components including clay minerals and oxides. As weathering intensity …

The Australian continent is actively deforming in response to far-field stresses generated by
plate boundary interactions and buoyancy forces associated with mantle dynamics. On the …

Despite its importance, the temporal and spatial evolution of continental dynamic
topography is poorly known. Australia's isolation from active plate boundaries and its rapid …

Despite its importance, the spatial and temporal pattern of dynamic topography generated
by mantle convective circulation is poorly known. We present accurate estimates of dynamic …

Classical geomorphological models identify regional erosion surfaces and raise
hypotheses, currently abandoned but largely untested, about the cumulative effects of …

One of the world's largest internally drained (endorheic) basins, the 1.14 million km 2 Lake
Eyre (hydrological) Basin (LEB), covers nearly 15% of the Australian continent …

The deployment of seismic stations and the development of ambient noise tomography as
well as new analysis methods provide an opportunity for higher-resolution imaging of …

The geological evolution of Australia is closely linked to supercontinent cycles that have
characterised the tectonic evolution of Earth, with most geological and metallogenic events …