The greater part of the metamorphic record of the Yilgarn Craton formed during a protracted middle Neoarchaean orogenic cycle, spanning from about 2750 to 2620 Ma. At least six …
In order to better understand continental growth history, we have determined the U–Pb age of about 1500 detrital zircons from river sands in three major rivers in North America and …
The Capricorn Orogen was initiated during Palaeoproterozoic suturing events that brought together the Archaean Yilgarn and Pilbara cratons to form the West Australian Craton. The …
A regional tectonic model is presented for the formation and evolution of Paleoproterozoic basins over the northern Yilgarn Craton, integrating new and published regional geological …
Abstract The Central Indian Tectonic Zone (CITZ) is a Proterozoic suture along which the Northern and Southern Indian Blocks are inferred to have amalgamated forming the Greater …
The Capricorn Orogen in central Western Australia records the Palaeoproterozoic collision of the Archaean Pilbara and Yilgarn Cratons. Until recently only one orogenic event was …
The Proterozoic igneous, deformation and metamorphic histories of the Palaeoproterozoic Rudall Complex in the northwestern Paterson Orogen can be linked to those of the Arunta …
AS Goldberg - Journal of Geodynamics, 2010 - Elsevier
The six large fanning dyke swarms mapped here using aeromagnetic data span two periods in the evolution of the Columbia supercontinent:(i) 1.9–1.7 Ga during and immediately …
Palaeoproterozoic granitic rocks of the Dalgaringa Supersuite dominate the Glenburgh Terrane, which forms the southern part of the Gascoyne Complex in the Capricorn Orogen …