A Mission to Very Early Earth: When Did Conditions Suitable for Life Emerge on Earth? A uniquely Australian resource - 4.4-4.1 Ga detrital zircons from the Jack Hills (WA) - represent the only tangible record of the Hadean Eon (4.5-4.0 Ga) and potentially contain information regarding the origin of the atmosphere, hydrosphere, continental lithosphere, geodynamo, and perhaps even life, during the earliest stages of Earth evolution. Following age characterization of 100,000 zircons, experiments in ....A Mission to Very Early Earth: When Did Conditions Suitable for Life Emerge on Earth? A uniquely Australian resource - 4.4-4.1 Ga detrital zircons from the Jack Hills (WA) - represent the only tangible record of the Hadean Eon (4.5-4.0 Ga) and potentially contain information regarding the origin of the atmosphere, hydrosphere, continental lithosphere, geodynamo, and perhaps even life, during the earliest stages of Earth evolution. Following age characterization of 100,000 zircons, experiments involving short-lived nuclear chronometers and tracers of continental evolution (Hf and O isotopes) will be undertaken on the most ancient zircons that could both radically our paradigm for early planetary evolution and permit assessment of whether life emerged during the Hadean Eon.Read moreRead less
Distribution and origin of 4 billion-year-old zircons from Western Australia: Implications for the early history of the earth and moom. We aim to determine the distribution and origin of >4 billion year old (Ga) zircons in rocks from north-western Western Australia, using geological mapping, mineralogical and chemical techniques and SHRIMP zircon geochronology. The >4Ga zircons are the oldest known crustal material, and the only material which can give direct information on the earliest evoluti ....Distribution and origin of 4 billion-year-old zircons from Western Australia: Implications for the early history of the earth and moom. We aim to determine the distribution and origin of >4 billion year old (Ga) zircons in rocks from north-western Western Australia, using geological mapping, mineralogical and chemical techniques and SHRIMP zircon geochronology. The >4Ga zircons are the oldest known crustal material, and the only material which can give direct information on the earliest evolution of the Earth. In this research, we will collaborate with international research groups also intending to investigate the early history of the Earth using the >4Ga zircons. Outcomes will be new ideas on the origin of the zircons, the differentiation of the Earth, the formation of the Moon and the Earth's oceans, and the development of ancient life forms.Read moreRead less
Mapping Under the Ice - crustal evolution in Antarctica and the assembly of Gondwanaland. The project will use a novel approach to map the sub-ice geology of Antarctica, and fill a gap in paleogeographical reconstructions. Paleocurrents indicate that Permo-Triassic river sands in Gondwanaland were dispersed from the sub-glacial Gamburtsev Mountains and the Beardmore-Ross region following the collision of Gondwanaland and Laurussia to form Pangea. An integrated U-Pb and Hf-isotope analysis of zi ....Mapping Under the Ice - crustal evolution in Antarctica and the assembly of Gondwanaland. The project will use a novel approach to map the sub-ice geology of Antarctica, and fill a gap in paleogeographical reconstructions. Paleocurrents indicate that Permo-Triassic river sands in Gondwanaland were dispersed from the sub-glacial Gamburtsev Mountains and the Beardmore-Ross region following the collision of Gondwanaland and Laurussia to form Pangea. An integrated U-Pb and Hf-isotope analysis of zircon grains from these sandstones will map the age and crustal evolution of these intracontinental orogens. Comparison with similar data from older Devonian sands in Australia-Antarctica-Africa will allow reconstruction of the pre- and post-collisional tectonics of Australia and adjoining areas of Gondwanaland.Read moreRead less
Discovery Early Career Researcher Award - Grant ID: DE190101011
Funder
Australian Research Council
Funding Amount
$380,000.00
Summary
Deep-sea magnetics: a key tool for enhanced 4D hydrothermal exploration. This project aims to constrain the magnetic response and detectability of mantle and hotspot-related vents. Deep-sea hydrothermal systems are oases of unique life and are considered as the most valuable scientific and mining targets ever discovered in the oceans. The project is expected to enable a better understanding of these enigmatic features, in both their active and inactive phases. It will use new and highly powerful ....Deep-sea magnetics: a key tool for enhanced 4D hydrothermal exploration. This project aims to constrain the magnetic response and detectability of mantle and hotspot-related vents. Deep-sea hydrothermal systems are oases of unique life and are considered as the most valuable scientific and mining targets ever discovered in the oceans. The project is expected to enable a better understanding of these enigmatic features, in both their active and inactive phases. It will use new and highly powerful processing methods on existing data and on data collected off the Tasmanian continental shelf. The project is expected to unveil the characteristics of hydrothermalism in a wide range of contexts and improve Australia’s competitiveness in scientific and mining hydrothermal exploration and to potentially guarantee the supply of raw materials for future generations.Read moreRead less
Realising Australia’s rare earth resource potential. This project aims to reveal the potential for undiscovered economic deposits of rare earth elements within the Australian continent. Future supply of these elements underpins societies transition to clean energy and embrace of high-tech applications. The project expects to greatly enhance our knowledge of Australia’s endowment of rare earth element resources using an array of traditional and innovative geological research methods. Expected out ....Realising Australia’s rare earth resource potential. This project aims to reveal the potential for undiscovered economic deposits of rare earth elements within the Australian continent. Future supply of these elements underpins societies transition to clean energy and embrace of high-tech applications. The project expects to greatly enhance our knowledge of Australia’s endowment of rare earth element resources using an array of traditional and innovative geological research methods. Expected outcomes of this project include a greater understanding of how, where and when rare earth element orebodies form in the Earth's crust. This should provide significant benefits to exploring for––and discovering––new orebodies that are required to secure global critical metal supplies. 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
The Rare Earth Potential of the Gascoyne Region of Western Australia. The Gascoyne Region of Western Australia is an emerging Neodymium-rich rare earth district in its early stages of development. The mineral occurrences of the region are complex and their geological distribution and source(s) remain unclear. With the support of all the active explorers in the region, a better understanding of the entire mineral system is sought to maximise exploration efficiency. This project aims to undertake ....The Rare Earth Potential of the Gascoyne Region of Western Australia. The Gascoyne Region of Western Australia is an emerging Neodymium-rich rare earth district in its early stages of development. The mineral occurrences of the region are complex and their geological distribution and source(s) remain unclear. With the support of all the active explorers in the region, a better understanding of the entire mineral system is sought to maximise exploration efficiency. This project aims to undertake a full assessment of the minerals, their processing and the environmental impact of production to determine the potential of the region. The expected outcome of the project is to develop a world-class rare earth mineral district in Australia, to ensure future supplies of these strategically important metals. Read moreRead less
An experimental study of trace element equilibria during metamorphism. The analytical methods and experimental data to be developed will enable an Australian team to become world leaders in determining pressures and temperatures of mineral growth that correspond to a range of depths and temperature gradients in the Earth tha t is wider than accessible previously. Obtaining this information from small zones within single grains will allow determination of rates of change, and give us a detailed p ....An experimental study of trace element equilibria during metamorphism. The analytical methods and experimental data to be developed will enable an Australian team to become world leaders in determining pressures and temperatures of mineral growth that correspond to a range of depths and temperature gradients in the Earth tha t is wider than accessible previously. Obtaining this information from small zones within single grains will allow determination of rates of change, and give us a detailed picture of how the host rock has evolved, even from very small samples. One application would be checking the origin of relatively common minerals for whether they could be associated with diamonds.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
Discovery Early Career Researcher Award - Grant ID: DE240100654
Funder
Australian Research Council
Funding Amount
$468,367.00
Summary
Critical metal fluid migration in shear zones during tectonic switches. This project aims to investigate why critical metal ore deposits form in inverted shear zones, which are zones of deformation that result from tectonic plates moving away from then towards each other. Numerical modelling of inverted shear zones will reveal drivers of ore fluid migration and will be combined with investigation of mineralised and non-mineralised inverted shear zones. This project will generate a new understand ....Critical metal fluid migration in shear zones during tectonic switches. This project aims to investigate why critical metal ore deposits form in inverted shear zones, which are zones of deformation that result from tectonic plates moving away from then towards each other. Numerical modelling of inverted shear zones will reveal drivers of ore fluid migration and will be combined with investigation of mineralised and non-mineralised inverted shear zones. This project will generate a new understanding of how inverted shear zones pump fluids through rocks to cause enrichment and ore deposition. This type of deposit is common in Queensland and the expected outcomes are improved exploration models, leading to discovery of new ore deposits, which is pivotal as the global demand for critical metals increases.Read moreRead less