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 …

Although major crustal lineaments may play an important role in mineralisation, the
relationship between lineaments and mineral deposits can be quite cryptic, and structural …

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 …

The precise timing and nature of the final assembly of the supercontinent Nuna, marked by
the collision of proto-Australia and Laurentia (North America) between 1.65 and 1.50 Ga …

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 …

Tectonic models for the latest Paleoproterozoic to earliest Mesoproterozoic evolution of
eastern Australia (circa 1620–1500 Ma) are diverse and either emphasize plume or plate …

Divergent genetic models have been proposed for clastic dominant (CD-type) massive
sulfide Zn-Pb mineralization in the Proterozoic Carpentaria Zn Province. Due to varying …

The Selwyn Zone is characterized by multiple ductile deformation and metamorphic events.
There is general consensus that early in the Isan Orogeny there were both extensional and …