Mapping Under the Ice - crustal evolution in Antarctica and the assembly of Gondwanaland. The project will use a novel approach to map the sub-ice geology of Antarctica, and fill a gap in paleogeographical reconstructions. Paleocurrents indicate that Permo-Triassic river sands in Gondwanaland were dispersed from the sub-glacial Gamburtsev Mountains and the Beardmore-Ross region following the collision of Gondwanaland and Laurussia to form Pangea. An integrated U-Pb and Hf-isotope analysis of zi ....Mapping Under the Ice - crustal evolution in Antarctica and the assembly of Gondwanaland. The project will use a novel approach to map the sub-ice geology of Antarctica, and fill a gap in paleogeographical reconstructions. Paleocurrents indicate that Permo-Triassic river sands in Gondwanaland were dispersed from the sub-glacial Gamburtsev Mountains and the Beardmore-Ross region following the collision of Gondwanaland and Laurussia to form Pangea. An integrated U-Pb and Hf-isotope analysis of zircon grains from these sandstones will map the age and crustal evolution of these intracontinental orogens. Comparison with similar data from older Devonian sands in Australia-Antarctica-Africa will allow reconstruction of the pre- and post-collisional tectonics of Australia and adjoining areas of Gondwanaland.Read moreRead less
From Synchrotron Characterisation of Single Fluid Inclusions to Archaean Geodynamics: An Integrated Study of Fluid-Rock Interaction in the Primitive Crust. In the primitive Earth, a wide range of phenomena including the initiation of biological activity and the formation of ore deposits were related to the mobilisation of mineralised fluids through the crust. In the Archaean craton of the Pilbara (WA), we have identified, within its tectonic framework, a crustal-scale plumbing system that channe ....From Synchrotron Characterisation of Single Fluid Inclusions to Archaean Geodynamics: An Integrated Study of Fluid-Rock Interaction in the Primitive Crust. In the primitive Earth, a wide range of phenomena including the initiation of biological activity and the formation of ore deposits were related to the mobilisation of mineralised fluids through the crust. In the Archaean craton of the Pilbara (WA), we have identified, within its tectonic framework, a crustal-scale plumbing system that channelled large volumes of mineralised hydrothermal solutions. Our objective is to understand the development of this plumbing system in relation to Archaean crustal geodynamics using a combination of structural geology, metamorphic petrology, geochronology, geochemistry, and the analysis of single-fluid inclusion using synchrotron and other X-ray sources.Read moreRead less