RB 2012/00017 Transpression and lower crustal extrusion: a transect across the Paleoproterozoic Kalinjala Shear System in the south-eastern Gawler Craton.
Published: 01 Nov 2012
Created: 25 Nov 2024
Revised: 27 Nov 2024
Author: Hand, M.P.;Reid, A.J.;Dutch, R.A.;Lane, K.;Jagodzinski, E.A.
The Gawler Craton preserves a tectonic history spanning the interval c. 3200 – 1400 Ma, and its evolution is dominated by Neoarchean to Mesoproterozoic tectonic events. Prior to the Jurassic-Cretaceous breakup of Australia and Antarctica, the...
The Gawler Craton preserves a tectonic history spanning the interval c. 3200 – 1400 Ma, and its evolution is dominated by Neoarchean to Mesoproterozoic tectonic events. Prior to the Jurassic-Cretaceous breakup of Australia and Antarctica, the Gawler Craton was part of a larger continental entity, the Mawson Continent. Central to developing earth crustal paleogeographic reconstructions that involve the Gawler Craton, or to generating predictive models for its metallogenesis, is the requirement that involved researchers have a detailed understanding of the stratigraphic and tectonic events milestones which are preserved within it. The subject field trip conducted within the south-eastern Gawler Craton was designed to highlight known major variations in lithostratigraphic composition and to examine the rock evidence of cycles of orogenic and magmatic reworking believed to have occurred therein.
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