The response of groundwater recharge to climate change needs to be understood to enable
sustainable management of groundwater systems today and in the future, yet observations …

The Australian and Indian plates are unique in that their absolute plate motion rates have
been much higher than those of any other plates which include a large continent. Changes …

The Perth Basin constitutes one of the principal tectonic features along the western
continental margin of Australia and formed through Permo-Cretaceous rifting of Greater …

Fossil pollen and spores preserved in organic‐rich claystones near the base of the
palaeochannel hosting the Tertiary Yandi channel iron deposits (CID) provide an in situ …

The intracratonic Canning Basin is Western Australia's largest sedimentary basin (> 400 000
km2) and has experienced repeated episodes of Phanerozoic extension and subsidence …

Satellite altimetry has revolutionised our knowledge of the tectonic structure of the ocean
floor and the continental shelves where ship data are sparse. We have used existing and …

Shallow-marine methane seeps, described here for the first time from the Australian Upper
Paleozoic, are among few reported globally from the Carboniferous–Permian. Carbonate …

Restoration of interpreted 2D deep seismic lines across Australia's North West Shelf
indicates that rifting style changed significantly during multiple phases of extension and …

The Carnarvon Basin of Western Australia is a rift basin that contains a thick (up to 5 km)
succession of late Carboniferous–early Permian glacially influenced marine sedimentary …

The longest interval of cold climate in Earth's Phanerozoic history spanned some 55 million
years from the Namurian (late Carboniferous) to the Kungurian (early Permian) when …