Multiscale geomechanical modelling of basin-scale CO2 storage. This project aims to develop innovative geomechanical models that will provide rapid assessments of the potential for reservoir deformation, including induced seismicity, during geological storage of CO2. The main expected outcome is a multiscale modelling approach that will help to identify storage locations at low risk for deformation and CO2 leakage in regions of little existing geomechanical data. The project will elucidate the .... Multiscale geomechanical modelling of basin-scale CO2 storage. This project aims to develop innovative geomechanical models that will provide rapid assessments of the potential for reservoir deformation, including induced seismicity, during geological storage of CO2. The main expected outcome is a multiscale modelling approach that will help to identify storage locations at low risk for deformation and CO2 leakage in regions of little existing geomechanical data. The project will elucidate the technical and commercial viability of CO2 storage in Australia’s Cooper-Eromanga basins and provide broad economic and environmental benefits by reducing the geomechanical uncertainties that provide a barrier to the global need to upscale carbon capture and storage.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
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