Tetconic feedback and the long-term evolution of the continents. The continents are shaped through complex interactions between the primary tectonic processes of magmatism, metamorphism, deformation, erosion and sedimentation. Because these processes modify the distribution of heat producing elements, and are themselves temperature sensitive, they must be subject to important feedback loops. This project will use constraints on heat producing element distributions in the Australian crust, and th ....Tetconic feedback and the long-term evolution of the continents. The continents are shaped through complex interactions between the primary tectonic processes of magmatism, metamorphism, deformation, erosion and sedimentation. Because these processes modify the distribution of heat producing elements, and are themselves temperature sensitive, they must be subject to important feedback loops. This project will use constraints on heat producing element distributions in the Australian crust, and the way in which these distributions have evolved during various tectonic processes, to elucidate the nature and significance of "tectonic feedback" and its role in shaping the continents.Read moreRead less
The Early Stages of Granite Evolution: Extraction and Transport Through Ductile Crust . This research is aimed at understanding how the continents develop through several stages of rock melting. Rock melts deep in the continents to form granite magmas which rise, transporting to the upper crust important metals, such as gold, copper and tin, and heat producing elements such as uranium, thorium and potassium. This research proposal seeks to understand how granite melts form and rise transporting ....The Early Stages of Granite Evolution: Extraction and Transport Through Ductile Crust . This research is aimed at understanding how the continents develop through several stages of rock melting. Rock melts deep in the continents to form granite magmas which rise, transporting to the upper crust important metals, such as gold, copper and tin, and heat producing elements such as uranium, thorium and potassium. This research proposal seeks to understand how granite melts form and rise transporting these all important elements, which control not only our wealth but also the stability of the continents we live in.Read moreRead less
An experimental exploration of silicate melt therrmodynamics. The chemical properties of magmas are the key to understanding igneous activity in the Earth, and hence the tectonic significance of magmatism, and the mineral resources resulting from past magmatism. The chemistry of magmas is also a determining factor in assessing the hazards associated with volcanic eruptions, including natural inputs into the atmosphere against which anthropogenic inputs causing climate change must be assessed. Th ....An experimental exploration of silicate melt therrmodynamics. The chemical properties of magmas are the key to understanding igneous activity in the Earth, and hence the tectonic significance of magmatism, and the mineral resources resulting from past magmatism. The chemistry of magmas is also a determining factor in assessing the hazards associated with volcanic eruptions, including natural inputs into the atmosphere against which anthropogenic inputs causing climate change must be assessed. This research program will measure experimentally the way different magma compositions affect the solubilites of important volatile and trace-element components in magmas, providing the much-needed fundamental data to model magmatic activity.Read moreRead less
Mapping Fluid Flow in the Earth's Crust: a Li and B micro-isotopic and thermodynamic study of serpentinisation. Interaction of fluids with magnesium-rich rocks creates new minerals and, on a global scale, affects the physical and chemical evolution of the Earth. On a more local scale, such fluid: rock interactions can lock up carbon dioxide via the formation of carbonate minerals. However, the extent to which such reactions may self-propagate is unclear. A primary benefit of this study will b ....Mapping Fluid Flow in the Earth's Crust: a Li and B micro-isotopic and thermodynamic study of serpentinisation. Interaction of fluids with magnesium-rich rocks creates new minerals and, on a global scale, affects the physical and chemical evolution of the Earth. On a more local scale, such fluid: rock interactions can lock up carbon dioxide via the formation of carbonate minerals. However, the extent to which such reactions may self-propagate is unclear. A primary benefit of this study will be new constraints on the viability of magnesium-rich rocks in geosequestration applications. Additional benefits will be provided by the development of advanced new analytical methodologies, and an increased level of understanding of the way that fluid flow can modify nickel sulphide ore bodies.Read moreRead less
Volatile recycling at the crust-mantle interface: Evidence from halogens and noble gases in deep-crustal fluids. 1) The technique proposed for this study is of proven interest to the mineral exploration industry. This project will: i) increase knowledge of the deep-crustal fluids often implicated in giant hydrothermal ore deposits; and ii) develop laser ablation, which will increase the techniques applicability to Australia's oldest ore deposits. These outcomes will further benefit the mineral e ....Volatile recycling at the crust-mantle interface: Evidence from halogens and noble gases in deep-crustal fluids. 1) The technique proposed for this study is of proven interest to the mineral exploration industry. This project will: i) increase knowledge of the deep-crustal fluids often implicated in giant hydrothermal ore deposits; and ii) develop laser ablation, which will increase the techniques applicability to Australia's oldest ore deposits. These outcomes will further benefit the mineral exploration industry.
2) The experimental data can be applied to testing the long-term storage of CO2 by geo-sequestration.
3) The proposed research is extremely topical and will be presented at international conferences and in high impact journals raising the profile of Australian science. Read moreRead less
Global Lithospheric Architecture Mapping II. The continents have been rifted, or broken up, and collided, or re-assembled, along major zones of weakness many times throughout Earth's history. Boundaries between such continental domains focus large-scale movements of fluids that can produce giant ore deposits. This study will provide new perspectives on the localisation of world-class economic deposits, the Earth resources on which society depends. Innovations in imaging the deep Earth beneath co ....Global Lithospheric Architecture Mapping II. The continents have been rifted, or broken up, and collided, or re-assembled, along major zones of weakness many times throughout Earth's history. Boundaries between such continental domains focus large-scale movements of fluids that can produce giant ore deposits. This study will provide new perspectives on the localisation of world-class economic deposits, the Earth resources on which society depends. Innovations in imaging the deep Earth beneath continents, and in numerical modelling, will maintain our high international profile in research relevant to National Priority 1.6 (Developing Deep Earth Resources). Unique 3D geological maps of regions down to 250km will make the composition of deep Earth regions newly accessible to geoscientists and all potential endusers.Read moreRead less
Magmatic processes, volatiles and ore formation. A major current source of Australia's export wealth derives from mining of gold and copper ores. Many of our largest ore deposits, such as those at Mt Isa and Broken Hill, formed in paleo- environments equivalent to the active submarine volcanic arcs which we are proposing to study. Modern systems yield the vital clues to explore intelligently for fossil equivalents. We propose a two-pronged approach in world-renowned analytical and experimental l ....Magmatic processes, volatiles and ore formation. A major current source of Australia's export wealth derives from mining of gold and copper ores. Many of our largest ore deposits, such as those at Mt Isa and Broken Hill, formed in paleo- environments equivalent to the active submarine volcanic arcs which we are proposing to study. Modern systems yield the vital clues to explore intelligently for fossil equivalents. We propose a two-pronged approach in world-renowned analytical and experimental laboratories to understand active processes that will guide experimental simulations under controlled conditions. Results are critical for national economic advantage and the maintenance of Australian Earth science in the forefront of global research effort.
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Crustal Growth in the Northern Tasmanides. The Australian and Queensland governments have invested over $3 million to undertake deep crustal seismic imaging in northern Queensland, providing an extensive new geophysical dataset capable of modelling crustal architecture and geological evolution to unprecedented levels. However, such models will remain untested unless the data is groundtruthed by analysis of rocks at the surface, providing a geological framework for extrapolation into the deep Ea ....Crustal Growth in the Northern Tasmanides. The Australian and Queensland governments have invested over $3 million to undertake deep crustal seismic imaging in northern Queensland, providing an extensive new geophysical dataset capable of modelling crustal architecture and geological evolution to unprecedented levels. However, such models will remain untested unless the data is groundtruthed by analysis of rocks at the surface, providing a geological framework for extrapolation into the deep Earth. The framework critically describes when and how crustal blocks were assembled, and the integrated information will generate evolutionary 3D models that will substantially improve mineral exploration targeting in the region.Read moreRead less
Sulfide Partial Melting at Broken Hill: Process and Implications. Based entirely on experimental studies, we suggested that the sulfide ore at Broken Hill, N.S.W., partially melted during granulite-facies metamorphism. Our subsequent discovery of sulfide melt inclusions in silicates associated with the ore strongly supports this assertion. This proposed research will evaluate the extent of melting and the composition of such a melt as well as the effect of this melt on the rocks surrounding the ....Sulfide Partial Melting at Broken Hill: Process and Implications. Based entirely on experimental studies, we suggested that the sulfide ore at Broken Hill, N.S.W., partially melted during granulite-facies metamorphism. Our subsequent discovery of sulfide melt inclusions in silicates associated with the ore strongly supports this assertion. This proposed research will evaluate the extent of melting and the composition of such a melt as well as the effect of this melt on the rocks surrounding the ore. The results of this basic research will not only impact on Broken Hill genetic models specifically, but could profoundly effect our understanding of metamorphic and magmatic sulfide deposits globally.Read moreRead less
CO2-brine behaviour in high temperature geological processes: Microanalysis and significance. This project clearly lies within the national research priority of developing deep earth resources. It may strengthen our economic fabric through mineral deposit discoveries in Australia as well as other circum-Pacific countries. The proposed research will also indirectly enhance our understanding of the relationships between geosphere, biosphere, fluids and global greenhouse warming. By strong national ....CO2-brine behaviour in high temperature geological processes: Microanalysis and significance. This project clearly lies within the national research priority of developing deep earth resources. It may strengthen our economic fabric through mineral deposit discoveries in Australia as well as other circum-Pacific countries. The proposed research will also indirectly enhance our understanding of the relationships between geosphere, biosphere, fluids and global greenhouse warming. By strong national and international collaborations and our use of innovative frontier technologies of fluid microgeochemistry, we will expand recognition of Australia's world-class research capacities.Read moreRead less