Discovery Early Career Researcher Award - Grant ID: DE210101126
Funder
Australian Research Council
Funding Amount
$416,419.00
Summary
Stability of accessory minerals during low temperature geological processes. The project aims to improve Australia’s ability to discover mineral deposits beneath sedimentary basins by determining whether detrital accessory minerals in sedimentary basins can be an effective exploration tool. This project expects to generate new knowledge on the stability of detrital accessory minerals in the sedimentary cycle using observations from natural rocks and laboratory experiments. Expected outcomes incl ....Stability of accessory minerals during low temperature geological processes. The project aims to improve Australia’s ability to discover mineral deposits beneath sedimentary basins by determining whether detrital accessory minerals in sedimentary basins can be an effective exploration tool. This project expects to generate new knowledge on the stability of detrital accessory minerals in the sedimentary cycle using observations from natural rocks and laboratory experiments. Expected outcomes include an assessment of the accessory minerals that are best suited to exploration vectoring studies in sedimentary basins. This should provide significant benefits to government and industry by improving mineral exploration methods and also has implications for geochronology and provenance studies.Read moreRead less
Discovery Early Career Researcher Award - Grant ID: DE240101283
Funder
Australian Research Council
Funding Amount
$361,000.00
Summary
Linking Australia’s basement and cover mineral systems . The aim of this research is to use revolutionary new mineral-dating techniques to test the hypothesis that low-temperature fluids can transport metals from Australia's richly endowed geological basement to form new mineral deposits in the sedimentary basins that cover most of the continent. Sedimentary-hosted mineral systems are the largest source of the critical metal cobalt and the second largest source of copper on Earth. These two meta ....Linking Australia’s basement and cover mineral systems . The aim of this research is to use revolutionary new mineral-dating techniques to test the hypothesis that low-temperature fluids can transport metals from Australia's richly endowed geological basement to form new mineral deposits in the sedimentary basins that cover most of the continent. Sedimentary-hosted mineral systems are the largest source of the critical metal cobalt and the second largest source of copper on Earth. These two metals are essential to developing the green energy infrastructure and technologies that underpin a net zero economy. The expected outcomes are a detailed record of paleo-fluid flow and metal cycling in Australia's highly prospective sedimentary basins. 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
Discovery Early Career Researcher Award - Grant ID: DE230101642
Funder
Australian Research Council
Funding Amount
$357,299.00
Summary
Earth’s mid-life crisis: recipe for a habitable planet? This project aims to establish the state and nature of the physical Earth systems (climate, topography, geography, erosion, carbon cycle, oxygen cycle) during the Neoproterozoic Era that made our planet habitable to complex life. By analysing these systems together, fundamental drivers and contributions to making a habitable planet will be untangled. Expected outcomes include the first ever series of climate models of this time period, as w ....Earth’s mid-life crisis: recipe for a habitable planet? This project aims to establish the state and nature of the physical Earth systems (climate, topography, geography, erosion, carbon cycle, oxygen cycle) during the Neoproterozoic Era that made our planet habitable to complex life. By analysing these systems together, fundamental drivers and contributions to making a habitable planet will be untangled. Expected outcomes include the first ever series of climate models of this time period, as well a series of digital reconstructions of the physical systems themselves. Sedimentary hosted ore deposits, such as copper and cobalt, are formed partly as a function of erosion and climate, allowing us to provide a mechanistic driver to their formation, and consequently exploration.Read moreRead less
Measuring mantle hydrogen to map ore fluids and model plate tectonics. The goal of this project is to use magnetotellurics to measure mantle hydrogen content to aid in the discovery of new mineral deposits. Hydrogen controls the strength of Earth’s mantle and is a vital component of the systems that form giant ore deposits. However, mantle hydrogen content is unconstrained. Ore-forming fluids hydrate the mantle pathways on which they travel. The first aim of this project is to image these fluid ....Measuring mantle hydrogen to map ore fluids and model plate tectonics. The goal of this project is to use magnetotellurics to measure mantle hydrogen content to aid in the discovery of new mineral deposits. Hydrogen controls the strength of Earth’s mantle and is a vital component of the systems that form giant ore deposits. However, mantle hydrogen content is unconstrained. Ore-forming fluids hydrate the mantle pathways on which they travel. The first aim of this project is to image these fluid pathways to improve mineral exploration techniques. Plate tectonic models assume that the lithospheric mantle is dehydrated but existing data from magnetotellurics and mantle rocks show high hydrogen contents. The second aim of this project is to create a map of the hydrogen content of the plates, which may lead to new models for continental evolution and mantle dynamics.Read moreRead less
Realising Australia’s rare earth resource potential. This project aims to reveal the potential for undiscovered economic deposits of rare earth elements within the Australian continent. Future supply of these elements underpins societies transition to clean energy and embrace of high-tech applications. The project expects to greatly enhance our knowledge of Australia’s endowment of rare earth element resources using an array of traditional and innovative geological research methods. Expected out ....Realising Australia’s rare earth resource potential. This project aims to reveal the potential for undiscovered economic deposits of rare earth elements within the Australian continent. Future supply of these elements underpins societies transition to clean energy and embrace of high-tech applications. The project expects to greatly enhance our knowledge of Australia’s endowment of rare earth element resources using an array of traditional and innovative geological research methods. Expected outcomes of this project include a greater understanding of how, where and when rare earth element orebodies form in the Earth's crust. This should provide significant benefits to exploring for––and discovering––new orebodies that are required to secure global critical metal supplies. Read moreRead less
The carbonate geology of the critical metal niobium. This project aims to understand how pyrochlore, the major ore mineral of the critical metal niobium, forms in
Earth’s crust. Niobium is exclusively mined from carbonatite magma bodies in Brazil and Canada, despite proven
Australian resources. It is used in high strength steel alloys in the construction and transport industries. Expected
research outcomes include understanding how pyrochlore forms in carbonatites, development of exploration too ....The carbonate geology of the critical metal niobium. This project aims to understand how pyrochlore, the major ore mineral of the critical metal niobium, forms in
Earth’s crust. Niobium is exclusively mined from carbonatite magma bodies in Brazil and Canada, despite proven
Australian resources. It is used in high strength steel alloys in the construction and transport industries. Expected
research outcomes include understanding how pyrochlore forms in carbonatites, development of exploration tools
to locate niobium ore bodies which are unexposed at the surface, and investigation of environmentally and
economically sustainable technologies for metallurgical extraction of niobium from ore. The research is intended
to benefit Australia’s critical metals exploration and mining industries.Read moreRead less
Eruption dynamics and tsunami potential from submarine volcanoes. This project is based on recently acquired seafloor samples and geophysical data from extraordinary deposits at a modern submarine volcano. This project aims to determine the conditions that lead to explosive eruption underwater, the dynamics of associated sediment flows, and if these events can trigger tsunami. Expected outcomes include an unprecedented reconstruction of the architecture of submarine caldera volcanoes, new innova ....Eruption dynamics and tsunami potential from submarine volcanoes. This project is based on recently acquired seafloor samples and geophysical data from extraordinary deposits at a modern submarine volcano. This project aims to determine the conditions that lead to explosive eruption underwater, the dynamics of associated sediment flows, and if these events can trigger tsunami. Expected outcomes include an unprecedented reconstruction of the architecture of submarine caldera volcanoes, new innovative models applicable globally for a richer understanding of volcanic tsunami and eruptions that shape the seafloor. This project will provide significant benefits through mitigation of global marine natural hazards, and by improving knowledge on the volcanic hosts of ore deposits.Read moreRead less
Impact of melt loss on crustal heat production and Earth geodynamics. This project plans to develop a thermodynamic tool set to calculate the amounts of rare earth elements, thorium and uranium in monazite and link its growth and radiogenic heat budget to rock evolution. Thorium (Th) and uranium (U) produce 83 per cent of the heat in Earth’s continental crust. Vast tracts of high-heat-producing rock from hot, deep parts of the crust defy the notion that such crust is depleted in Th and U. The ca ....Impact of melt loss on crustal heat production and Earth geodynamics. This project plans to develop a thermodynamic tool set to calculate the amounts of rare earth elements, thorium and uranium in monazite and link its growth and radiogenic heat budget to rock evolution. Thorium (Th) and uranium (U) produce 83 per cent of the heat in Earth’s continental crust. Vast tracts of high-heat-producing rock from hot, deep parts of the crust defy the notion that such crust is depleted in Th and U. The causes of high heat production in the deep crust remain unclear. This project will develop a tool set to calculate the Th and U concentration in minerals (eg monazite, zircon) and silicate melt as a function of depth, temperature and rock composition. This tool set would be of great benefit to the geoscience community for better understanding fundamental geodynamic processes.Read moreRead less
Breaking Gondwana: interplay between tectonics, climate and resources. The project aims to reconstruct 250 million years of landscape evolution in response to rifting and break-up of the Gondwana supercontinent, using the innovative approach of combining regional thermochronology with global plate tectonic models. From these reconstructions, the time-integrated record of exhumation and erosion at the continental margins will be revealed at an unprecedented scale. The main expected outcome will b ....Breaking Gondwana: interplay between tectonics, climate and resources. The project aims to reconstruct 250 million years of landscape evolution in response to rifting and break-up of the Gondwana supercontinent, using the innovative approach of combining regional thermochronology with global plate tectonic models. From these reconstructions, the time-integrated record of exhumation and erosion at the continental margins will be revealed at an unprecedented scale. The main expected outcome will be a deep time archive of the relationships between tectonic forcing, continental erosion and the global climate, which may assist predictions and debate on future climate change. The outcomes will also provide economic benefits as they will inform on the exhumation and preservation of (critical) mineral resources.Read moreRead less