In recent years several tectonic reconstructions have been presented for Australia–
Antarctica break-up, with each putting the Australian plate in a different location with respect …

Tectonic influences on long-term climate change are of considerable current interest and
debate. This paper reviews the relationship between multi-million year periods of glaciation …

Pangea results from the progressive amalgamation of continental blocks achieved at 320
Ma. Assuming that the ancient concept of “active” versus “passive” rifting remains pertinent …

Abstract Since 2007/2008, seismographs were deployed in many new locations across
much of Antarctica. Using the records from 122 broadband seismic stations, over 10,000 …

The second generation Antarctic magnetic anomaly compilation for the region south of 60° S
includes some 3.5 million line‐km of aeromagnetic and marine magnetic data that more than …

Intracontinental alkaline complexes and carbonatites commonly occur in rift-related settings,
best exemplified by the Cenozoic–present day East African Rift System. Examples in the …

Wildfire has been implicated as a potential driver of deforestation and continental
biodiversity loss during the end-Permian extinction event (EPE;∼ 252 Ma). However, it …

The formation and disruption of supercontinents exert major influence on mantle dynamics
and have important bearing on continental dynamics and mineral systems. Here we …

Timor Island, in the Outer Banda Arc, bordering the Timor Sea, preserves the orogenic
product of an arc–continent collision between the Australian Plate and the Banda Arc that …

In the Prince Charles Mountains (PCMs) the conformable Permian–Triassic (P–T)
succession is characterised by an abrupt transition from coal-bearing to coal-lacking strata …