Geological and paleomagnetic data support the hypothesis that a Paleo-Mesoproterozoic
supercontinent, referred to as Columbia, existed before the formation of Rodinia. This pre …

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 …

Abstract The Savannah (formerly Sally Malay) Ni-Cu-Co Camp is composed of a group of
mineralised intrusions (Savannah and Savannah North) and petrologically similar mafic …

The evolution of the Australian plate can be interpreted in a plate‐tectonic paradigm in
which lithospheric growth occurred via vertical and horizontal accretion. The lithospheric …

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 …

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 …

Abstract The Musgrave Block in central southern Australia separates the dominantly
Paleoproterozoic North Australian Craton from the Late Archean to early Mesoproterozoic …

By virtue of its large area of exposure of different crustal levels, and preservation of a
protracted (∼ 400 million years) Palaeoproterozoic to Mesoproterozoic tectonic evolution …

A global survey of sutures predating formation of the supercontinent Rodinia, ie, older than
ca. 0.9–1.0 Ga, has yielded evidence for at least 35 described and possible ophiolite …

The Palaeoproterozoic ca. 1620–1608Ma St Peter Suite, located in the central Gawler
Craton, South Australia comprises mafic to felsic magmatic rocks. The intermediate to felsic …