Linkage Infrastructure, Equipment And Facilities - Grant ID: LE200100035
Funder
Australian Research Council
Funding Amount
$610,000.00
Summary
WA CRC-MC-ICPMS for Earth, Planetary and Environmental science. This Application aims to provide a mass spectrometer for Australian researchers collaborating on NASA, Japanese Aerospace Exploration Agency and China National Space Administration extra-terrestrial sample return missions as they characterise unique samples of dust and rock collected from asteroids, the Moon and meteorites. The Application will also support government geoscience agencies who will generate nationally significant isot ....WA CRC-MC-ICPMS for Earth, Planetary and Environmental science. This Application aims to provide a mass spectrometer for Australian researchers collaborating on NASA, Japanese Aerospace Exploration Agency and China National Space Administration extra-terrestrial sample return missions as they characterise unique samples of dust and rock collected from asteroids, the Moon and meteorites. The Application will also support government geoscience agencies who will generate nationally significant isotopic datasets to improve mineral exploration success, and scientists monitoring Earth’s environment. Expected outcomes will ensure that Australia remains at the forefront of cosmochemistry, minerals research and environmental studies, which will provide significant benefits to our economy and society.
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Linkage Infrastructure, Equipment And Facilities - Grant ID: LE100100064
Funder
Australian Research Council
Funding Amount
$450,000.00
Summary
A facility for sensitive and precise isotopic dating of the earth's and extraterrestrial rocks. SPIDE2R will be a new generation mass spectrometer for very precise and sensitive dating and forensics applications in earth and planetary sciences, hydrology, climate studies, and nuclear and archaeological fingerprinting. The unprecedented sensitivity of this unique instrument will provide enhanced capabilities for solving long-standing problems requiring precise geological time resolution, as well ....A facility for sensitive and precise isotopic dating of the earth's and extraterrestrial rocks. SPIDE2R will be a new generation mass spectrometer for very precise and sensitive dating and forensics applications in earth and planetary sciences, hydrology, climate studies, and nuclear and archaeological fingerprinting. The unprecedented sensitivity of this unique instrument will provide enhanced capabilities for solving long-standing problems requiring precise geological time resolution, as well as opening new areas of research. It will be the instrument of choice for analysing small, rare samples such as those returned by space missions. The Australian-built high sensitivity source and ion detection systems can be retrofitted onto other mass spectrometers, opening a new area of commercialisation.Read moreRead less
Accessory Mineral Microstructure and Implications for Geochronology. U-Pb geochronology of accessory minerals is widely used to constrain the timing of igneous, metamorphic and sedimentary processes. However, our current knowledge of isotope mobility in these important minerals cannot readily explain some common features of U-Pb dating. Using new developments in quantitative microstructural analysis integrated with high spatial resolution geochronology we will constrain the relationship between ....Accessory Mineral Microstructure and Implications for Geochronology. U-Pb geochronology of accessory minerals is widely used to constrain the timing of igneous, metamorphic and sedimentary processes. However, our current knowledge of isotope mobility in these important minerals cannot readily explain some common features of U-Pb dating. Using new developments in quantitative microstructural analysis integrated with high spatial resolution geochronology we will constrain the relationship between accessory minerals deformation and its effect on radiometric ages. Our results will lead to a better understanding of geochemical modification of accessory minerals and may lead to the development of new applications of geochronology and improve the dating of rock deformation.Read moreRead less
Discovery Early Career Researcher Award - Grant ID: DE190101307
Funder
Australian Research Council
Funding Amount
$421,824.00
Summary
A new nano-geochronology approach to global Earth processes. This project aims to develop a new nano-geochronology tool. Geochronology is the science of determining the ages of rocks and geological events, and is key to answering fundamental questions of planetary evolution, the geological processes that shaped our Earth, and evolution of life and past climates. Many valuable mineral phases are too small to be dated by conventional methods. The potential that nano-geochronology has to unlock inf ....A new nano-geochronology approach to global Earth processes. This project aims to develop a new nano-geochronology tool. Geochronology is the science of determining the ages of rocks and geological events, and is key to answering fundamental questions of planetary evolution, the geological processes that shaped our Earth, and evolution of life and past climates. Many valuable mineral phases are too small to be dated by conventional methods. The potential that nano-geochronology has to unlock information otherwise untraceable remains largely unexplored. The development and application of nano-geochronology will improve our understanding of the Australian crust and the field of geological mapping, which largely supports mineral exploration.Read moreRead less
Mineral reaction, deformation, and accessory phases in migmatites: What controls monazite behaviour during high-grade metamorphism? Isotopic dating of rocks and minerals has revolutionized the way we view our planet, and allowed us to attach an absolute timescale to a range of Earth processes from the evolution of life to formation of mineral deposits. Australian technology has long been at the forefront of this field, but it is apparent that our ability to date Earth materials has overtaken our ....Mineral reaction, deformation, and accessory phases in migmatites: What controls monazite behaviour during high-grade metamorphism? Isotopic dating of rocks and minerals has revolutionized the way we view our planet, and allowed us to attach an absolute timescale to a range of Earth processes from the evolution of life to formation of mineral deposits. Australian technology has long been at the forefront of this field, but it is apparent that our ability to date Earth materials has overtaken our ability to interpret these ages in terms of geologic processes. The results of this study and the associated collaboration will ensure that Australian understanding of what isotopic ages mean keeps pace with our ability to measure them. This will allow us to resolve finer details of Earth history, and improve our understanding of the planet and how best to manage it.Read moreRead less
Proterozoic tectonic evolution of Australia and India. Recent studies cast doubt on reconstructions of the Neoproterozoic supercontinent Rodinia, and on the tectonic coherence of East Gondwanaland (Australia, Antarctica and India). Within Australia, the relative positions of the major crustal blocks during most of the Proterozoic era remain largely unverified. Fossil magnetism in rocks of different ages from the major crustal blocks of Australia and India will be used to determine whether the ....Proterozoic tectonic evolution of Australia and India. Recent studies cast doubt on reconstructions of the Neoproterozoic supercontinent Rodinia, and on the tectonic coherence of East Gondwanaland (Australia, Antarctica and India). Within Australia, the relative positions of the major crustal blocks during most of the Proterozoic era remain largely unverified. Fossil magnetism in rocks of different ages from the major crustal blocks of Australia and India will be used to determine whether the blocks were together or were separated by large oceans during Proterozoic time. The results will place fundamental constraints on the geological, palaeogeographic, and palaeobiological evolution of Australia, Rodinia, and the early Earth as a whole.Read moreRead less
Accessory REE-phosphates as tracers of heat and fluids in time and space. This project will provide fundamental information vital for the widespread application of a new and developing technique for dating rocks and ore bodies that formed at geologically low temperatures. The technique will benefit the Australian mining industry by improving models for the formation of ore deposits, thereby reducing the financial risk involved in discovering new resources. Results will highlight the value of ano ....Accessory REE-phosphates as tracers of heat and fluids in time and space. This project will provide fundamental information vital for the widespread application of a new and developing technique for dating rocks and ore bodies that formed at geologically low temperatures. The technique will benefit the Australian mining industry by improving models for the formation of ore deposits, thereby reducing the financial risk involved in discovering new resources. Results will highlight the value of another Australian invention - the SHRIMP - in resolving both fundamental and applied geological problems, encouraging the uptake of this technology overseas. Outcomes from this project will enhance Australia's scientific reputation as a world leader in geochronology and economic geology.Read moreRead less
Precise global time scale for the oxidation of Earth's atmosphere between 2.6 and 2.0 billion years ago. The rock record from 2600 to 2000 million years ago preserves evidence for dramatically fluctuating greenhouse and icehouse climates at the same time as, and possibly caused by, change from an oxygen-deficient to an oxygen-rich atmosphere. Although the global changes are well-documented, correlation of their timing and duration between continents is poorly constrained. This project aims to re ....Precise global time scale for the oxidation of Earth's atmosphere between 2.6 and 2.0 billion years ago. The rock record from 2600 to 2000 million years ago preserves evidence for dramatically fluctuating greenhouse and icehouse climates at the same time as, and possibly caused by, change from an oxygen-deficient to an oxygen-rich atmosphere. Although the global changes are well-documented, correlation of their timing and duration between continents is poorly constrained. This project aims to redress that problem by producing a precise calibration of the global changes by analysis of the rock records in Australia, Canada and South Africa. It will provide a much needed time framework within which long-term feedback between atmospheric composition and climate can be understood.Read moreRead less
A Pan African-aged suture zone in western Madagascar: Tracking the lost Mozambique Ocean. The aims of the project are to identify and locate a major suture in western Madagascar i.e, between Africa and Madagascar. The precise age of this suture will ba dated using U/Pb zircon geochronology, Ar / Ar analysis combined with on-site fieldwork. The project also aims to provide a coherent geotectonic framework for the Madagascar microcontinent both north and south of the Ranotsara Shear Zone. The p ....A Pan African-aged suture zone in western Madagascar: Tracking the lost Mozambique Ocean. The aims of the project are to identify and locate a major suture in western Madagascar i.e, between Africa and Madagascar. The precise age of this suture will ba dated using U/Pb zircon geochronology, Ar / Ar analysis combined with on-site fieldwork. The project also aims to provide a coherent geotectonic framework for the Madagascar microcontinent both north and south of the Ranotsara Shear Zone. The project has significant implications for the reconstruction and continental configuration of both Gondwanaland and Rodinia.Read moreRead less
The ins and outs of a Proterozoic supercontinent - what is the significance of 990-900 Ma orogenesis for the assembly of Rodinia? The hypothesis that all of Earth's continents came together one billion years ago to form a supercontinent known as Rodinia has invigorated debate about ancient continental distributions. Current models depict a flawed configuration for Rodinia, since they assume that continental fragments preserving evidence for quite different episodes of tectonic activity between ....The ins and outs of a Proterozoic supercontinent - what is the significance of 990-900 Ma orogenesis for the assembly of Rodinia? The hypothesis that all of Earth's continents came together one billion years ago to form a supercontinent known as Rodinia has invigorated debate about ancient continental distributions. Current models depict a flawed configuration for Rodinia, since they assume that continental fragments preserving evidence for quite different episodes of tectonic activity between 1350 and 900 million years ago developed at the same time. This project will make new correlations based upon careful observation and precise isotopic dating of rocks in Antarctica and Mexico, and will use these data to develop a more realistic picture of the ancient Earth.Read moreRead less