From exploration to mining: new geological strategies for sustaining high levels of copper production from the Mount Isa district. Mineral production at the Mount Isa copper and Ernest Henry copper-gold mines is worth more than $ 1 billion per year and this has underpinned the northern Queensland economy for a number of years. These resources are being depleted at a high rate, and no significant new discoveries have been made in over a decade. This project will provide some of the tools to defin ....From exploration to mining: new geological strategies for sustaining high levels of copper production from the Mount Isa district. Mineral production at the Mount Isa copper and Ernest Henry copper-gold mines is worth more than $ 1 billion per year and this has underpinned the northern Queensland economy for a number of years. These resources are being depleted at a high rate, and no significant new discoveries have been made in over a decade. This project will provide some of the tools to define new resources for the next generation, ensuring the prosperity of the region and bolstering the Australian economy. The timing is critical given the long lead time between discovery and production (in the order of 5 to 10 years). If successful the research may have major financial impacts at local, regional and national scales. It may also improve mine safety.Read moreRead less
Evolution of the Proterozoic lithosphere and its bearing of sediment hosted base metal mineralisation. This project aims to determine the aspects of lithospheric evolution that led to a concentration of giant base metal mineral deposits in the Early to Middle Proterozoic (ca 1.9-1.5 billion years ago). We propose to test three related hypotheses that, if validated, will fundamentally change our view of Proterozoic metallogenesis and the way the mineral industry approaches exploration for these ....Evolution of the Proterozoic lithosphere and its bearing of sediment hosted base metal mineralisation. This project aims to determine the aspects of lithospheric evolution that led to a concentration of giant base metal mineral deposits in the Early to Middle Proterozoic (ca 1.9-1.5 billion years ago). We propose to test three related hypotheses that, if validated, will fundamentally change our view of Proterozoic metallogenesis and the way the mineral industry approaches exploration for these deposits.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
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
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
Isotopic fractionation in ore metals (Cu, Fe and Zn): A new window on ore-forming processes. Stable isotopes of common ore metals (e.g, copper and iron) are new tools for investigating ore deposits. Our data suggest that metal isotopic variations can provide new insights into mechanisms operative during formation of ore deposits. Stable metal isotopes also show promise as a new exploration tool for identifying the location of economic mineralisation within large prospective terrains; e.g., weakl ....Isotopic fractionation in ore metals (Cu, Fe and Zn): A new window on ore-forming processes. Stable isotopes of common ore metals (e.g, copper and iron) are new tools for investigating ore deposits. Our data suggest that metal isotopic variations can provide new insights into mechanisms operative during formation of ore deposits. Stable metal isotopes also show promise as a new exploration tool for identifying the location of economic mineralisation within large prospective terrains; e.g., weakly vs. strongly mineralised zones in a volcanic belt.
This project will provide fundamental baseline data that will help elucidate the processes that cause metal isotope variations. This will allow stable metal isotopes to be used much more effectively by the mining and exploration industries.
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Transitions and Zoning in Porphyry-Epithermal Districts: Indicators, Discriminators, and Vectors. We aim to improve understanding of ore genesis and exploration success in porphyry-epithermal mineral districts. These districts can contain porphyry Cu-Mo-Au deposits (the world's major source of copper), epithermal Au-Ag deposits, skarn and sediment-hosted gold deposits. These districts continue to be important targets for copper and gold explorers, even though it can be difficult to identify th ....Transitions and Zoning in Porphyry-Epithermal Districts: Indicators, Discriminators, and Vectors. We aim to improve understanding of ore genesis and exploration success in porphyry-epithermal mineral districts. These districts can contain porphyry Cu-Mo-Au deposits (the world's major source of copper), epithermal Au-Ag deposits, skarn and sediment-hosted gold deposits. These districts continue to be important targets for copper and gold explorers, even though it can be difficult to identify the ore zones within large zones of background alteration. We will develop and test criteria that can be used by explorers to indicate prospective environments, discriminate between mineralization styles, and vector towards ore zones - be they of porphyry, epithermal, and/or other peripheral styles.Read moreRead less
Mobility of metals in hydrothermal solutions: critical experiments and numerical modelling tools to improve exploration success and ore processing. After more than 100 years of intense prospecting, ore deposits with a surface expression or a characteristic geophysical signature have been discovered. As a result, the industry needs innovative and quantitative exploration techniques. Geochemical exploration suffers from a growing gap between ever more powerful geochemical analytical capabilities a ....Mobility of metals in hydrothermal solutions: critical experiments and numerical modelling tools to improve exploration success and ore processing. After more than 100 years of intense prospecting, ore deposits with a surface expression or a characteristic geophysical signature have been discovered. As a result, the industry needs innovative and quantitative exploration techniques. Geochemical exploration suffers from a growing gap between ever more powerful geochemical analytical capabilities and the poor understanding of fundamental processes in hydrothermal systems. By combining new experiments on important geochemical systems (association between the trace elements Te and As with Au) with advances in numerical modelling of H2O-CO2-NaCl fluids, the project aims to bring geochemical exploration in line with geophysical exploration.Read moreRead less
Genetic and chemical characterisation of the pristine Archean Jaguar base-metal deposit, to improve local and global prospectivity. Jaguar is a remarkably pristine finely banded submarine volcanic hosted base-metals-silver deposit from the Australian Archean, ~2.7 billion years old. We will document its detailed ore and volcanic textures, gaining valuable new genetic insights from its extraordinary preservation. With an emerging mining company in regional Western Australia, we will combine foren ....Genetic and chemical characterisation of the pristine Archean Jaguar base-metal deposit, to improve local and global prospectivity. Jaguar is a remarkably pristine finely banded submarine volcanic hosted base-metals-silver deposit from the Australian Archean, ~2.7 billion years old. We will document its detailed ore and volcanic textures, gaining valuable new genetic insights from its extraordinary preservation. With an emerging mining company in regional Western Australia, we will combine forensic textural studies with advanced geochemical analysis to (1) determine the deposit origin; (2) infer the origin of other well laminated but less well preserved deposits globally; (3) apply these findings to the detection of local prospective horizons under deep cover; and (4) use the deposit features to test current models of massive sulfide formation.Read moreRead less
What controls trace element levels in ore sulfides? A laser-ICPMS perspective. Sub-surface hydrothermal gold and base metal orebodies are surrounded by aprons of elevated metal concentrations, mainly within micro-sulfides, which is one sign mineral explorers use to widen their target. Here we test whether the hostrock contributes metal in the most distant parts of such halos, and if so, what factors control where hostrock metal begins to be detectable in a given system. We will make better model ....What controls trace element levels in ore sulfides? A laser-ICPMS perspective. Sub-surface hydrothermal gold and base metal orebodies are surrounded by aprons of elevated metal concentrations, mainly within micro-sulfides, which is one sign mineral explorers use to widen their target. Here we test whether the hostrock contributes metal in the most distant parts of such halos, and if so, what factors control where hostrock metal begins to be detectable in a given system. We will make better models of how metalliferous waters react with rock, potentially translating into million dollar savings through more efficient exploration. The ultrafine sampling and precision analyses required for this are possible because of an ARC-funded core program at CODES.Read moreRead less