Pyrite: a deep-time capsule of ocean chemistry and atmosphere oxidation. Surprisingly little is known about trace element trends in past oceans, even though these data are vital for interpreting the evolution of the Earth's atmosphere, evolutionary pathways of marine life and cycles of major mineral deposits. Using laser-based analysis of sedimentary pyrite in deep marine rocks, this project aims to produce, for the first time, temporal variation curves for 25 trace elements in seawater over the ....Pyrite: a deep-time capsule of ocean chemistry and atmosphere oxidation. Surprisingly little is known about trace element trends in past oceans, even though these data are vital for interpreting the evolution of the Earth's atmosphere, evolutionary pathways of marine life and cycles of major mineral deposits. Using laser-based analysis of sedimentary pyrite in deep marine rocks, this project aims to produce, for the first time, temporal variation curves for 25 trace elements in seawater over the last 3.5 billion years. Preliminary research has validated the technique and demonstrated major changes in certain trace elements over geologically short periods. Outcomes will assist the minerals industry in the discovery of new deposits of zinc, copper, gold and iron ore in Australia.Read moreRead less
Earth's best-preserved Archean boninites: do they finally resolve the Archean mantle plume - plate tectonics controversy? Subduction typically starts on the modern Earth with the eruption of chemically distinctive rocks known as boninites. This project will study remarkably well preserved 2.85 billion year old boninites from Western Australia that may finally establish whether modern-style plate tectonics operated in the first half of Earth's history.
Where to find giant porphyry and epithermal gold and copper deposits. This project will determine when and where giant gold or copper deposits should form, consolidating links with Indonesia, and using South East Asia as a vast natural laboratory in which to examine the effect of large-scale tectonic processes. The project will produce a four-dimensional virtual exploration toolkit to show how to apply the methods.
Evolution of sub-arc mantle oxidation state over Earth’s history. This project aims to determine how the oxidation state of the Earth's mantle has changed throughout geologic history in response to recycling of sulfur, carbon and iron though subduction zones, and how this has influenced mineral deposit formation. The expected outcome is a holistic model that ties evolution of the Earth's biosphere to geochemical changes in the deep Earth that control mineral deposit formation. By improving our u ....Evolution of sub-arc mantle oxidation state over Earth’s history. This project aims to determine how the oxidation state of the Earth's mantle has changed throughout geologic history in response to recycling of sulfur, carbon and iron though subduction zones, and how this has influenced mineral deposit formation. The expected outcome is a holistic model that ties evolution of the Earth's biosphere to geochemical changes in the deep Earth that control mineral deposit formation. By improving our understanding of how, where, when and why mineral deposits formed, this project should provide improvements in mineral exploration strategy, and thus benefits to Australia's economy.Read moreRead less
Discovery Early Career Researcher Award - Grant ID: DE150101190
Funder
Australian Research Council
Funding Amount
$350,259.00
Summary
The role of hydrostatic pressure in modulating submarine silicic eruptions. Exploration on the modern seafloor reveals the deposits of deep (greater than 1 000 metres) silicic explosive eruptions, yet theory predicts that explosivity at these depths is largely suppressed. In 2012 the largest and deepest silicic submarine explosive eruption ever recorded took place at depths up to 1 600 metres, also challenging this theory. This project leverages a United States of America research expedition to ....The role of hydrostatic pressure in modulating submarine silicic eruptions. Exploration on the modern seafloor reveals the deposits of deep (greater than 1 000 metres) silicic explosive eruptions, yet theory predicts that explosivity at these depths is largely suppressed. In 2012 the largest and deepest silicic submarine explosive eruption ever recorded took place at depths up to 1 600 metres, also challenging this theory. This project leverages a United States of America research expedition to the eruption site. This project aims to constrain the physical and chemical factors that control explosivity using cutting-edge technologies. Australia's ancient submarine volcanoes host highly economic ore deposits. This project aims to enhance the ability to interpret ancient volcanic settings, thereby improving the potential for new ore deposit discoveries.Read moreRead less
The copper-gold fertility of mountain belts. This project aims to identify the timing of, and understand the causes of, sulphide saturation in granitic suites to test the hypothesis that sulphide saturation controls the fertility of copper-gold deposits. More than half of the world’s copper and gold comes from granitic rocks, but most granitic suites are barren. As copper-gold deposits become increasingly difficult to find, and exploration budgets have been slashed, it is critical to reliably di ....The copper-gold fertility of mountain belts. This project aims to identify the timing of, and understand the causes of, sulphide saturation in granitic suites to test the hypothesis that sulphide saturation controls the fertility of copper-gold deposits. More than half of the world’s copper and gold comes from granitic rocks, but most granitic suites are barren. As copper-gold deposits become increasingly difficult to find, and exploration budgets have been slashed, it is critical to reliably distinguish ore bearing from barren systems. Platinum group element geochemistry could make this distinction by pinpointing the timing of sulphide saturation in evolving magma systems. Eliminating barren suites as exploration targets will save Australia’s exploration dollars which can be directed to where the prospects of success are greatest.Read moreRead less
Four dimensional lithospheric evolution and controls on mineral system distribution in Neoarchean to Paleoproterozoic terranes. This project will resolve important questions about the links between the evolution and preservation of continents and important mineral deposits in Australia and West Africa between 2.7 and 1.8 billion years ago. The results will improve the understanding of a key period of Earth history and make a major contribution to mineral exploration.
Exploration targeting from next-generation volcanic facies reconstruction. The project aims to develop new innovative image analysis techniques to reconstruct the architecture of the volcanic host at four highly prospective hydrothermal-magmatic ore deposits, and investigate the properties of rocks that favour high-grade ore mineralisation. Expected outcomes of this project include next-generation automated techniques for volcanic facies analysis, and predictions of where hydrothermal alteration ....Exploration targeting from next-generation volcanic facies reconstruction. The project aims to develop new innovative image analysis techniques to reconstruct the architecture of the volcanic host at four highly prospective hydrothermal-magmatic ore deposits, and investigate the properties of rocks that favour high-grade ore mineralisation. Expected outcomes of this project include next-generation automated techniques for volcanic facies analysis, and predictions of where hydrothermal alteration is most prospective for mineralisation. Both outcomes are relevant to the discovery of volcanic-hosted mineralisation globally. This project will provide significant benefit to the Australian mining industry by diversifying ore exploration strategies in the Australian crust, and will train the next generation of explorers.Read moreRead less
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
Fluid chemistry and critical mineral enrichment in salty metamorphic belts. Several geological regions in Australia are worth billions of dollars to our economy in their contained copper-goldcobalt and uranium-rare earth element mineral deposits. These regions will continue to be important to Australia as the world transitions to a renewable energy economy because they can provide some of the most critical metals needed for that transition: Cu, Co, rare earth elements. This project aims to provi ....Fluid chemistry and critical mineral enrichment in salty metamorphic belts. Several geological regions in Australia are worth billions of dollars to our economy in their contained copper-goldcobalt and uranium-rare earth element mineral deposits. These regions will continue to be important to Australia as the world transitions to a renewable energy economy because they can provide some of the most critical metals needed for that transition: Cu, Co, rare earth elements. This project aims to provide a fundamental quatitative understanding of the geological processes that form these deposits. We will conduct experiments to generate quantitative models of the metamorphic and structural processes that control the liberation and migration of highly saline fluids, which are ideal for transporting a large range of metals.Read moreRead less