The early tectonic evolution of the Curnamona Province. This project aims to test the hypothesis that the Curnamona Province preserves evidence for an extension-related structural geology architecture. This will allow a comparison of the basin evolution, crustal architecture and mechanisms of basin development between the Curnamona Province and well-understood basins of the Mount Isa Inlier. The project is expected to add value to pre-existing databases, and deliver a plate tectonic and str ....The early tectonic evolution of the Curnamona Province. This project aims to test the hypothesis that the Curnamona Province preserves evidence for an extension-related structural geology architecture. This will allow a comparison of the basin evolution, crustal architecture and mechanisms of basin development between the Curnamona Province and well-understood basins of the Mount Isa Inlier. The project is expected to add value to pre-existing databases, and deliver a plate tectonic and structural framework to interpret basin evolution and constrain geochronology/geochemical analysis, and develop a three-dimesional crustal architecture. The results will provide new constraints on the evolution of the Australian plate, and how the Australian crust has evolved.Read moreRead less
Time- and Temperature-Dependence of the Fluid Transport Properties, Strength and Mechanical Behaviour of Crustal Faults - An Experimental and Modelling Study. High temperature rock deformation experiments will be performed in conjunction with high resolution, computer-aided x-ray microtomography to determine time-dependent and temperature-dependent effects on fluid transport properties, strength and mechanical behaviour during slip and interseismic healing of simulated fault rocks in hydrotherma ....Time- and Temperature-Dependence of the Fluid Transport Properties, Strength and Mechanical Behaviour of Crustal Faults - An Experimental and Modelling Study. High temperature rock deformation experiments will be performed in conjunction with high resolution, computer-aided x-ray microtomography to determine time-dependent and temperature-dependent effects on fluid transport properties, strength and mechanical behaviour during slip and interseismic healing of simulated fault rocks in hydrothermal environments. The results will be used with cellular automaton modelling approaches to develop a quantitative understanding of how coupling between fluid flow and rock deformation controls earthquake rupture and fluid migration in fault networks in the continental seismogenic regime. This work will provide new understanding of triggers for earthquake nucleation and controls on localisation of ore deposits.Read moreRead less
Tectonic mode switches and the nature of orogenesis. Tectonic mode switches coincide with short periods of time during which base and precious metals, as well as diamond-bearing kimberlites are emplaced into the continental crust. Our research is aimed at uncovering why this should be so, thereby perhaps solving a riddle that is at the present little more than an oddity in respect to mineral exploration. If we can understand the underlying science we may be able to provide practical benefits t ....Tectonic mode switches and the nature of orogenesis. Tectonic mode switches coincide with short periods of time during which base and precious metals, as well as diamond-bearing kimberlites are emplaced into the continental crust. Our research is aimed at uncovering why this should be so, thereby perhaps solving a riddle that is at the present little more than an oddity in respect to mineral exploration. If we can understand the underlying science we may be able to provide practical benefits to mineral explorers. The project uses modelling and simulation research infrastructure provided by the AuScope NCRIS initiative, and benefits the community by returning data to this organization.Read moreRead less
Numerical modelling of deformation partitioning and its role in metamorphism, tectonism and mineralization. Targeting blind mineralization is the biggest problem facing the Australian mining industry. The modelling developed in this project will integrate deformation, fluid and chemical processes and provide a means for understanding the deformation partitioning that localizes epigenetic ore regionally as well as along portions of large-scale structures. Applying this to known ore deposits may ....Numerical modelling of deformation partitioning and its role in metamorphism, tectonism and mineralization. Targeting blind mineralization is the biggest problem facing the Australian mining industry. The modelling developed in this project will integrate deformation, fluid and chemical processes and provide a means for understanding the deformation partitioning that localizes epigenetic ore regionally as well as along portions of large-scale structures. Applying this to known ore deposits may delineate adjacent plus regionally distributed zones where the deformation event responsible for mineralization is locally present at sufficient intensity to form ore. This would allow targeted deep drilling in ground with no ore close to the surface saving millions in drilling costs and dramatically increasing the financial viability of this industry. Read moreRead less
Geologic, genetic and exploration implications of syndeformational, structurally-controlled, sediment-hosted copper deposits: investigation of the Mt Oxide deposit, Queensland. This project will use a multi-disciplinary approach to understand the geology, geochemistry and genesis of the syndeformational, structurally-controlled, sediment-hosted copper mineralisation at the Mt Oxide deposit, Queensland. Copper deposits, like Mt Oxide, are an important exploration target in sedimentary basins but ....Geologic, genetic and exploration implications of syndeformational, structurally-controlled, sediment-hosted copper deposits: investigation of the Mt Oxide deposit, Queensland. This project will use a multi-disciplinary approach to understand the geology, geochemistry and genesis of the syndeformational, structurally-controlled, sediment-hosted copper mineralisation at the Mt Oxide deposit, Queensland. Copper deposits, like Mt Oxide, are an important exploration target in sedimentary basins but their characteristics and formation are poorly understood. Discovery of further sediment-hosted Cu deposits is imperative as Australia's industrial competitivness in exploration and mining depends on the discovery of new ore depsoits. This project specifically addresses the need for better genetic and exploration models for copper deposits concealed within ancient, deformed sedimentary sequences in Australia and overseas.Read moreRead less
Defects and Deformation in Olivine: From Molecules to Mantle. This project establishes the role of hydrogen in controlling olivine deformation, plate tectonics and mantle geodynamics. The unique application of innovative nanoscale simulation, microscale observation and geophysical characterisation ensures that results will have far-reaching impact in the Australian and International Earth Science community. In particular, our results will enable greater understanding of water migration in the m ....Defects and Deformation in Olivine: From Molecules to Mantle. This project establishes the role of hydrogen in controlling olivine deformation, plate tectonics and mantle geodynamics. The unique application of innovative nanoscale simulation, microscale observation and geophysical characterisation ensures that results will have far-reaching impact in the Australian and International Earth Science community. In particular, our results will enable greater understanding of water migration in the mantle, the formation of deep Earth mineral resources and lead to significant improvements in the interpretation of geophysical variations in Earth's lithosphere.Read moreRead less
Origin and setting of Congolese-type Cu deposits. This project aims to understand the genesis of the giant sediment-hosted Cu ore deposits of the Congolese Copperbelt, and their relationship to the enclosing strata. We will use selected study areas within the correlative Neoproterozic basin successions in Australia, which are well exposed and covered by modern geoscientific datasets, as analogues for the poorly exposed Congolese system. Once this is achieved, we will combine the results with tho ....Origin and setting of Congolese-type Cu deposits. This project aims to understand the genesis of the giant sediment-hosted Cu ore deposits of the Congolese Copperbelt, and their relationship to the enclosing strata. We will use selected study areas within the correlative Neoproterozic basin successions in Australia, which are well exposed and covered by modern geoscientific datasets, as analogues for the poorly exposed Congolese system. Once this is achieved, we will combine the results with those of a previous ARC linkage project on the nearby Zambian Copperbelt, to provide the first integrated model of the worlds largest sedimentary Cu system.Read moreRead less
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
Physical and Chemical Constraints of Fluid Activated Processes During the Polyphase Tectonic Evolution of the Olary Domain, S.A. The Olary Domain, eastern South Australia, underwent several phases of deformation and metamorphism. These events mobilised fluids leading, amongst other features, to the formation of breccia bodies and mineral deposits. The complex nature of the geological evolution of the region obscures relationships of fluid migration to the structural history. Fluid inclusion stud ....Physical and Chemical Constraints of Fluid Activated Processes During the Polyphase Tectonic Evolution of the Olary Domain, S.A. The Olary Domain, eastern South Australia, underwent several phases of deformation and metamorphism. These events mobilised fluids leading, amongst other features, to the formation of breccia bodies and mineral deposits. The complex nature of the geological evolution of the region obscures relationships of fluid migration to the structural history. Fluid inclusion studies and stable isotope analyses combined with structural analyses on micro to macro scales shall establish links between the thermal and structural evolution of the area. This will provide insigth into the scale and physico-chemical characteristics of fluids and mineralising processes an relate these to the tectono-thermal history.Read moreRead less