The origin of the Antarctic continent can be traced to a relatively small late Archaean cratonic
nucleus centred on the Terre Adélie regions of East Antarctica and the Gawler Craton region …

Abstract Sediment-hosted Pb-Zn deposits can be divided into two major subtypes. The first
subtype is clastic-dominated lead-zinc (CD Pb-Zn) ores, which are hosted in shale …

Deep seismic reflection profiling confirms that the Paleo-to Mesoproterozoic Mount Isa
mineral province comprises three vertically stacked and partially inverted sedimentary …

The western two-thirds of Australia is underlain by Precambrian rocks that are divisible into
three Archean to Paleoproterozoic cratons, the West Australian, North Australian and South …

This paper presents a plate tectonic model for the evolution of the Australian continent
between ca. 1800 and 1100Ma. Between ca. 1800 and 1600Ma episodic orogenesis …

The Australian continent records c. 1860–1800 Ma orogenesis associated with rapid
accretion of several ribbon micro-continents along the southern and eastern margins of the …

Continental lithosphere formed and reworked during the Palaeoproterozoic era is a major
component of pre-1070 Ma Australia and the East Antarctic Shield. Within this lithosphere …

Palaeomagnetism of climatically sensitive sedimentary rock types, such as glacial deposits
and evaporites, can test the uniformitarianism of ancient geomagnetic fields and …

Abstract From the Mesoproterozoic to Cambrian, Australo-Antarctica was characterised by
tectonic reconfiguration as part of the supercontinents Columbia, Rodinia and Gondwana …

Over 500 zircon grains separated from modern sediments in 10 drainages covering the
Eastern Succession of the Mt Isa Inlier have been analysed for U–Pb ages, Hf isotopes, and …