Distribution and origin of 4 billion-year-old zircons from Western Australia: Implications for the early history of the earth and moom. We aim to determine the distribution and origin of >4 billion year old (Ga) zircons in rocks from north-western Western Australia, using geological mapping, mineralogical and chemical techniques and SHRIMP zircon geochronology. The >4Ga zircons are the oldest known crustal material, and the only material which can give direct information on the earliest evoluti ....Distribution and origin of 4 billion-year-old zircons from Western Australia: Implications for the early history of the earth and moom. We aim to determine the distribution and origin of >4 billion year old (Ga) zircons in rocks from north-western Western Australia, using geological mapping, mineralogical and chemical techniques and SHRIMP zircon geochronology. The >4Ga zircons are the oldest known crustal material, and the only material which can give direct information on the earliest evolution of the Earth. In this research, we will collaborate with international research groups also intending to investigate the early history of the Earth using the >4Ga zircons. Outcomes will be new ideas on the origin of the zircons, the differentiation of the Earth, the formation of the Moon and the Earth's oceans, and the development of ancient life forms.Read moreRead less
Fluid-induced creation and decay of porosity and permeability in minerals. This project aims to investigate the role of hydrothermal fluids in the creation and decay of porosity and permeability in minerals. By developing new experimental techniques and undertaking experimental studies mimicking natural conditions, this project expects to generate knowledge of the fundamental relationships between fluid-mineral reactions, pore creation and decay, pore geometry and connectivity, and the mechanism ....Fluid-induced creation and decay of porosity and permeability in minerals. This project aims to investigate the role of hydrothermal fluids in the creation and decay of porosity and permeability in minerals. By developing new experimental techniques and undertaking experimental studies mimicking natural conditions, this project expects to generate knowledge of the fundamental relationships between fluid-mineral reactions, pore creation and decay, pore geometry and connectivity, and the mechanism for the formation of fluid inclusions. This should provide significant benefits such as a deeper understanding of the hydrothermal fluids flowing through tight rocks in the Earth’s crust to form orebodies, and provide a scientific basis to underpin the development of greener technologies for recovering natural resources.Read moreRead less
Mapping mineral systems of deep Australia. We aim at enabling mineral resource discoveries by calibrating geophysical surveys using geochemical and petrophysical properties measured on mantle samples brought to the surface by recent volcanoes. National geophysical surveys deliver images of geophysical gradients in the deeper part of the Australian continent. The interpretation of these gradients in geological terms and in terms of economic mineral systems is the key to unlock deep exploration su ....Mapping mineral systems of deep Australia. We aim at enabling mineral resource discoveries by calibrating geophysical surveys using geochemical and petrophysical properties measured on mantle samples brought to the surface by recent volcanoes. National geophysical surveys deliver images of geophysical gradients in the deeper part of the Australian continent. The interpretation of these gradients in geological terms and in terms of economic mineral systems is the key to unlock deep exploration success. This project will turn Australia’s investment in National geophysical surveys into new discoveries of base metals. The benefit stems from enabling the transition to a clean economy which requires a much broader range of critical minerals and a larger quantity of base metals.Read moreRead less
Bio-recovery of rare earth elements from Australian soils and mine tailings. This project aims to discover how microbes dissolve weathering-resistant phosphate minerals that contain valuable rare earth elements used widely in modern technology. This discovery would create new knowledge in the interdisciplinary fields of biogeochemistry and biohydrometallurgy, using an innovative combination of techniques in metagenomics, microbiology and mineralogy. Expected research outcomes include new, more ....Bio-recovery of rare earth elements from Australian soils and mine tailings. This project aims to discover how microbes dissolve weathering-resistant phosphate minerals that contain valuable rare earth elements used widely in modern technology. This discovery would create new knowledge in the interdisciplinary fields of biogeochemistry and biohydrometallurgy, using an innovative combination of techniques in metagenomics, microbiology and mineralogy. Expected research outcomes include new, more economic and environmentally sustainable biotechnologies for recovering rare earth elements and increasing phosphorus availability in Australian mineral deposits and soils. These outcomes should benefit the mining and agricultural sectors, by decreasing Australia's dependency on overseas REE supply and the use of fertilizers.Read moreRead less
Multiple vertical tectonic movements in a continental interior: consequences of flat-subduction and foundering of an oceanic plateau? This project will investigate how the subduction of particularly thick oceanic crust impacts on the landscape, climate, structure and composition of the adjacent continent. It will help in understanding the history and distribution of mineral and hydrocarbon resources, of similar provinces in Australia.