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Deciphering the tectonic record of the early Earth. This project aims to decipher how and why plate tectonics emerged, and how any precursor tectonic system modulated planetary heat loss. The project expects to generate new knowledge regarding the tectonic record of the early Earth using pressure–temperature–age constraints from truly ancient (2.8–4.0 billion year old) metamorphosed rocks worldwide. Expected outcomes of this collaborative international project include the development of a concep ....Deciphering the tectonic record of the early Earth. This project aims to decipher how and why plate tectonics emerged, and how any precursor tectonic system modulated planetary heat loss. The project expects to generate new knowledge regarding the tectonic record of the early Earth using pressure–temperature–age constraints from truly ancient (2.8–4.0 billion year old) metamorphosed rocks worldwide. Expected outcomes of this collaborative international project include the development of a conceptual geodynamic model for the early Earth. This should provide significant benefits in permitting a better understanding of the where and why of Australia’s natural resources, in training a new generation of Earth system scientists, and in broadening public awareness of fundamental Earth science.
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Novel tools for dating explosive volcanic eruptions in the critical window. This project will develop novel dating methods necessary for precise reconstruction of the eruption histories of super-volcanoes in the Asia-Pacific region over the last million years. The project outcomes will provide better models for predicting super-eruptions, thereby informing global climate change research, urban planning, and transport and telecommunications infrastructure engineering. Results will also improve ex ....Novel tools for dating explosive volcanic eruptions in the critical window. This project will develop novel dating methods necessary for precise reconstruction of the eruption histories of super-volcanoes in the Asia-Pacific region over the last million years. The project outcomes will provide better models for predicting super-eruptions, thereby informing global climate change research, urban planning, and transport and telecommunications infrastructure engineering. Results will also improve existing volcanic risk models used by insurers to quantify volcanic risks and calculate expected losses from volcanic eruptions, and greatly improve our ability to use eruption deposits as time markers for important events in human evolution.Read moreRead less
Jurassic arc? Reconstructing the lost world of Eastern Australia. This project aims to resolve a long-standing enigma about the geological formation of the Great Artesian Basin – Australia’s most important onshore reservoir for groundwater and hydrocarbon resources. Specifically, the project will integrate sedimentological and geochemical studies to investigate the geodynamic configuration of Eastern Australia during the Jurassic Period of basin formation. The intended outcomes are an improved u ....Jurassic arc? Reconstructing the lost world of Eastern Australia. This project aims to resolve a long-standing enigma about the geological formation of the Great Artesian Basin – Australia’s most important onshore reservoir for groundwater and hydrocarbon resources. Specifically, the project will integrate sedimentological and geochemical studies to investigate the geodynamic configuration of Eastern Australia during the Jurassic Period of basin formation. The intended outcomes are an improved understanding of the evolution of the Australian continent and better knowledge of the formation of intercontinental sedimentary basins, which includes better assessment of their potential to contain hydrocarbon resources.Read moreRead less
Garnet speed dating: Innovation for fast tectonic problem solving. This project aims to develop and apply a novel way to rapidly date the mineral garnet within rocks using the analytical technique of laser ablation mass spectrometry to calculate Lutetium-Hafnium ages. Garnet is the most important mineral we have to determine the depths of burial and the temperatures rocks experienced during the tectonic processes that shaped the continents. Our novel in situ laser ablation method will allow ga ....Garnet speed dating: Innovation for fast tectonic problem solving. This project aims to develop and apply a novel way to rapidly date the mineral garnet within rocks using the analytical technique of laser ablation mass spectrometry to calculate Lutetium-Hafnium ages. Garnet is the most important mineral we have to determine the depths of burial and the temperatures rocks experienced during the tectonic processes that shaped the continents. Our novel in situ laser ablation method will allow garnet to be rapidly and easily dated, permitting routine collection of large age datasets for tectonic problem solving. It will also offer a rapid means to determine ages of garnet-bearing rocks across prospective mineral exploration regions, providing explorers with key exploration data.Read moreRead less
What goes on inside subduction zones? This project aims to decipher how rocks behave inside subduction zones. Subduction is a central tenant of plate tectonic theory and the project will test the hypothesis rocks can become trapped within giant long-lived eddies that circulate material within subduction zones. This international collaborative project will generate new knowledge regarding the time scales rocks can remain trapped inside subduction zones using pressure–temperature–age constraints f ....What goes on inside subduction zones? This project aims to decipher how rocks behave inside subduction zones. Subduction is a central tenant of plate tectonic theory and the project will test the hypothesis rocks can become trapped within giant long-lived eddies that circulate material within subduction zones. This international collaborative project will generate new knowledge regarding the time scales rocks can remain trapped inside subduction zones using pressure–temperature–age constraints from subducted rocks. We will use this information as a framework for numerical simulations of subduction zone behaviour. The project will provide significant benefits in training a new generation of Earth scientists, and in broadening public awareness of fundamental Earth science.Read moreRead less
Testing continental growth models with calcium and strontium isotopes. The Project aims to chart the evolution of the Earth’s primordial mantle and oceans between 3.75 and 2.8 billion years ago using calcium and strontium isotopes in ancient igneous and sedimentary rocks. A novel solution to the controversy over the timing and rate of growth of the Earth’s continents is expected. Anticipated outcomes include the establishment of innovative analytical tools for tracing geological and environmenta ....Testing continental growth models with calcium and strontium isotopes. The Project aims to chart the evolution of the Earth’s primordial mantle and oceans between 3.75 and 2.8 billion years ago using calcium and strontium isotopes in ancient igneous and sedimentary rocks. A novel solution to the controversy over the timing and rate of growth of the Earth’s continents is expected. Anticipated outcomes include the establishment of innovative analytical tools for tracing geological and environmental processes, and stronger collaborative links with premier research institutions abroad. The significant benefits of the Project include an enhanced understanding of the environment in which early life evolved, and fresh insight into the formation of the richly mineralized nucleus of the Australian continent. Read moreRead less
A detrital apatite archive to track crustal growth. This project will establish apatite as a new tool to study the evolution of the continental crust. The crust shaped the composition of the atmosphere and the oceans with consequences for the evolution of life through the availability of oxygen and nutrients. However, when and how the continental crust was generated remains a core question. Current models for continental crust development rely on the mineral zircon. However, zircons only record ....A detrital apatite archive to track crustal growth. This project will establish apatite as a new tool to study the evolution of the continental crust. The crust shaped the composition of the atmosphere and the oceans with consequences for the evolution of life through the availability of oxygen and nutrients. However, when and how the continental crust was generated remains a core question. Current models for continental crust development rely on the mineral zircon. However, zircons only record the history of evolved rocks. To address this bias we will use the mineral apatite which forms in less evolved rocks. We will develop a detrital apatite database of Pb-Nd (model) ages and integrate this with the zircon record to provide a more holistic description for how our planet developed.Read moreRead less
Uncovering the Chronology of Mars. This project aims to answer fundamental questions about the origin and evolution of the solar system by utilizing innovative machine learning techniques developed by our group. Starting with Mars, we will interrogate the highest resolution image data to automatically generate the ultimate resolution global age map. The expected outcomes of this project include determining the absolute ages of geologic processes on Mars to deliver a groundbreaking look at the ge ....Uncovering the Chronology of Mars. This project aims to answer fundamental questions about the origin and evolution of the solar system by utilizing innovative machine learning techniques developed by our group. Starting with Mars, we will interrogate the highest resolution image data to automatically generate the ultimate resolution global age map. The expected outcomes of this project include determining the absolute ages of geologic processes on Mars to deliver a groundbreaking look at the geology of another planet at the centimeter scale. A major benefit of this project will be enhancing Australia’s role as a leader in space and planetary science through this interdisciplinary, international collaboration across engineering, geology, computing, and chronology.Read moreRead less
Hidden geochemical treasure: apatite inclusions in zircon. This project aims to undertake high precision measurements of the isotopic composition of tiny apatite inclusions in the mineral zircon. This project will create a new isotopic data set to combine with age and isotope data for the host zircons in order to study the formation and evolution of the Earth's crust. Primary apatite inclusions represent a previously untapped treasury of pristine geochemical information made accessible by the la ....Hidden geochemical treasure: apatite inclusions in zircon. This project aims to undertake high precision measurements of the isotopic composition of tiny apatite inclusions in the mineral zircon. This project will create a new isotopic data set to combine with age and isotope data for the host zircons in order to study the formation and evolution of the Earth's crust. Primary apatite inclusions represent a previously untapped treasury of pristine geochemical information made accessible by the latest advances in micro-analytical and imaging technology. This information will be used to test models for the timing of formation of the first continents, to map continental growth over time, and to evaluate the origins of the Earth's oldest rocks and minerals and the environmental conditions on the early Earth.Read moreRead less