Ultra-hot Mesoproterozoic evolution of
intracontinental central Australia
Weronika Gorczyk a;Hugh Smithies b;Fawna Korhonen b;Heather Howard b;Raphael Quentin De Gromard b
【期刊名称】《地学前缘(英文版)》 【年(卷),期】2015(000)001
【摘要】The Musgrave Province developed at the nexus of the North, West and South Australian cratons and its Mesoproterozoic evolution incorporates a 100 Ma period of ultra-high temperature (UHT) meta-morphism from ca. 1220 to ca. 1120 Ma. This was accompanied by high-temperature A-type granitic magmatism over an 80 Ma period, sourced in part from mantle-derived components and emplaced as a series of pulsed events that also coincide with peaks in UHT metamorphism. The tectonic setting for this thermal event (the Musgrave Orogeny) is thought to have been intracontinental and the lithospheric architecture of the region is suggested to have had a major influence on the thermal evolution. We use a series of two dimensional, fully coupled thermo-mechanical-petrological numerical models to investi-gate the plausibility of initiating and prolonging UHT conditions under model setup conditions appro-priate to the inferred tectonic setting and lithospheric architecture of the Musgrave Province. The results support the inferred tectonic framework for the Musgrave
Ultra-hot Mesoproterozoic evolution of intracontinental central Australia
