A new approach to understanding the mechanisms and deep crustal controls of continental rifting. This research will directly examine the northern plate boundary of Australia, providing analogues for rift-related crustal processes that occurred throughout ancient Australia, consistent with Priority Goal 6 (Developing Deep Earth Resources) in the Designated National Research Priority Area: "An Environmentally Sustainable Australia". The scientific innovation represented by this project will help t ....A new approach to understanding the mechanisms and deep crustal controls of continental rifting. This research will directly examine the northern plate boundary of Australia, providing analogues for rift-related crustal processes that occurred throughout ancient Australia, consistent with Priority Goal 6 (Developing Deep Earth Resources) in the Designated National Research Priority Area: "An Environmentally Sustainable Australia". The scientific innovation represented by this project will help to maintain the leading position of Australian scientists in examining these issues. This project will be of direct relevance to energy exploration along Australia's passive margins (oil and gas) and will provide better constraints on the rifting process that will aid in our understanding of rift-related metallogenesis.Read moreRead less
High-P partial melting and melt escape from the lower crust: the evolution of a Cretaceous Island Arc, Fiordland NZ. Partial melting, melt segregation and magma transport are the main processes controlling change on Earth. Though there is clear evidence that even small melt fractions can segregate into large igneous bodies, our inability to directly observe active magma ascent means that there is not agreement on the mechanisms by which melt initially segregates, pools and ascends. This project ....High-P partial melting and melt escape from the lower crust: the evolution of a Cretaceous Island Arc, Fiordland NZ. Partial melting, melt segregation and magma transport are the main processes controlling change on Earth. Though there is clear evidence that even small melt fractions can segregate into large igneous bodies, our inability to directly observe active magma ascent means that there is not agreement on the mechanisms by which melt initially segregates, pools and ascends. This project will study well-exposed lower crustal rocks from the root of a long-lived Mesozoic island arc to resolve the mechanisms that controlled melt escape from, and extensive magma transport through deep crustal environments.Read moreRead less
The enigmatic link between crustal growth and supercontinent formation. This project links with major energy and resource initiatives from the Australian Government. It will provide detailed geological information that will help constrain our understanding of the deep structure of the Earth in northern and central Australia. This knowledge will assist in mineral and energy resource exploration of these highly prospective regions. The information will also link with other ARC-funded geological st ....The enigmatic link between crustal growth and supercontinent formation. This project links with major energy and resource initiatives from the Australian Government. It will provide detailed geological information that will help constrain our understanding of the deep structure of the Earth in northern and central Australia. This knowledge will assist in mineral and energy resource exploration of these highly prospective regions. The information will also link with other ARC-funded geological studies, to help understand how a large, but enigmatic, part of the Australian continental grew rapidly, almost 2 billion years ago.
Read moreRead less
A test for Pangean breakup models. This project addresses a core issue of planetary-geology, with project outcomes providing an unparalleled synthesis of global-scale Earth processes that highlight hitherto unsuspected links between peripheral orogenic systems and Pangean breakup. The project directly addresses the key problem 'How do the continents work?', outlined by the National Committee of Earth Sciences. It links internationally to [ERAS], a multi-national proposal to investigate accretion ....A test for Pangean breakup models. This project addresses a core issue of planetary-geology, with project outcomes providing an unparalleled synthesis of global-scale Earth processes that highlight hitherto unsuspected links between peripheral orogenic systems and Pangean breakup. The project directly addresses the key problem 'How do the continents work?', outlined by the National Committee of Earth Sciences. It links internationally to [ERAS], a multi-national proposal to investigate accretionary orogens through geologic time, and nationally via the seed-funded ARC Network (AEON) to ACcess, RSES (ANU) and with a National Key Centre, (GEMOC), with whom the University of Newcastle is a research partner. 2PhD projects are involved.Read moreRead less
Thallium isotopes: a novel geochemical tracer to map recycling in Earth's mantle. This project will transfer to Australia an advanced new methodology: the characterisation of thallium isotopic signatures in the mantle system introduced during recycling of crustal material. This will allow the tracking of fluid processes in the mantle system in a completely new way and will provide significant new information about the fluids that can percolate up from subduction zones. The source of most econo ....Thallium isotopes: a novel geochemical tracer to map recycling in Earth's mantle. This project will transfer to Australia an advanced new methodology: the characterisation of thallium isotopic signatures in the mantle system introduced during recycling of crustal material. This will allow the tracking of fluid processes in the mantle system in a completely new way and will provide significant new information about the fluids that can percolate up from subduction zones. The source of most economically interesting elements in the crust is from mantle-derived fluids, so their characterisation is critical to an understanding of the whole ore-forming process. Hence, this study will provide unique new information to apply to this important large-scale Earth problem.Read moreRead less
Mantle Melting Dynamics and the Influence of Recycled Components. This proposal is directly concerned with the continuing aim of building a sustainable Australia through knowledge of deep earth resources. The more we know about the processes of melting and melt and fluid migration the better we will be able to inform models for resource exploration and volcanic hazard mitigation. Uranium series isotopes are relevant to the very recent history of the planet (< 350 000 years) - time scales which a ....Mantle Melting Dynamics and the Influence of Recycled Components. This proposal is directly concerned with the continuing aim of building a sustainable Australia through knowledge of deep earth resources. The more we know about the processes of melting and melt and fluid migration the better we will be able to inform models for resource exploration and volcanic hazard mitigation. Uranium series isotopes are relevant to the very recent history of the planet (< 350 000 years) - time scales which are often overlooked. Application to mantle melting as described in this proposal may also have direct application to gold exploration in the Manus basin and elsewhere. It is to these techniques we must look if we are to understand the immediate past as a clue to the immediate future of our planet.Read moreRead less
Earth's Internal System: deep processes and crustal consequences. Outcomes will include significant new information about the structure and formation of the Earth's crust and the underlying mantle. An improved framework for interpreting the architecture of Australia and other continents will be directly relevant to exploration for world-class economic deposits, the Earth resources on which society depends. Innovations in geochemical technology and in the integration of information from geochemi ....Earth's Internal System: deep processes and crustal consequences. Outcomes will include significant new information about the structure and formation of the Earth's crust and the underlying mantle. An improved framework for interpreting the architecture of Australia and other continents will be directly relevant to exploration for world-class economic deposits, the Earth resources on which society depends. Innovations in geochemical technology and in the integration of information from geochemistry, geophysics and geodynamics will maintain our high international profile in research relevant to National Priority 1.6 (Developing Deep Earth Resources). The project and its interaction with the minerals industry will provide advanced Postgraduate training in a field critical to Australia's future.Read moreRead less
How has the continental lithosphere evolved? Processes of assembly, growth, transformation and destruction. We will use new in-situ analytical techniques, developed In-house, to date the formation and modification of specific volumes of the subcontinental lithospheric mantle, and to define the temporal and genetic relationships between mantle events and crustal formation. Quantitative modelling will investigate the geodynamic consequences of spatial and temporal variations in lithosphere composi ....How has the continental lithosphere evolved? Processes of assembly, growth, transformation and destruction. We will use new in-situ analytical techniques, developed In-house, to date the formation and modification of specific volumes of the subcontinental lithospheric mantle, and to define the temporal and genetic relationships between mantle events and crustal formation. Quantitative modelling will investigate the geodynamic consequences of spatial and temporal variations in lithosphere composition and thermal state. Magmatic products will be used to assess the roles of mantle plumes and delamination in construction of the lithosphere and xenolith studies will investigate the evolution of oceanic plateaus. The results will provide a framework for interpreting the architecture of lithospheric terranes and their boundaries.Read moreRead less
How has continental lithosphere evolved? Processes of assembly, growth, transformation and destruction. Novel in-situ analytical and dating techniques will be used on samples from the Earth's mantle and deep crust to define the processes by which the continents and their roots (to depths of 250 km) have been formed, modified or destroyed at different times throughout Earth's 4.6 billion year evolution. The role of oceanic plateaus and mantle plumes in building protocontinents or modifying lithos ....How has continental lithosphere evolved? Processes of assembly, growth, transformation and destruction. Novel in-situ analytical and dating techniques will be used on samples from the Earth's mantle and deep crust to define the processes by which the continents and their roots (to depths of 250 km) have been formed, modified or destroyed at different times throughout Earth's 4.6 billion year evolution. The role of oceanic plateaus and mantle plumes in building protocontinents or modifying lithospheric volumes will be evaluated. The results will provide a more robust framework for interpreting the architecture of Earth's lithosphere and will have relevance to the formation and location of resources such as Ni, PGEs, Au and diamonds.Read moreRead less
Crustal Evolution in Australia: Ancient and Young Terrains. The mechanisms of crustal growth and the processes of crust-mantle interaction will be studied in selected Archean, Proterozoic and Phanerozoic terrains in Australia, using a newly developed approach: the integrated, in-situ microanalysis of Hf and Pb isotopic composition and trace-element patterns in zircons from sediments and selected igneous bodies. The results will provide new information on the evolution of the Australian crust, w ....Crustal Evolution in Australia: Ancient and Young Terrains. The mechanisms of crustal growth and the processes of crust-mantle interaction will be studied in selected Archean, Proterozoic and Phanerozoic terrains in Australia, using a newly developed approach: the integrated, in-situ microanalysis of Hf and Pb isotopic composition and trace-element patterns in zircons from sediments and selected igneous bodies. The results will provide new information on the evolution of the Australian crust, with wider implications for the development of global crust and mantle reservoirs. The outcomes will define crustal evolution signatures related to regional-scale mineralisation, and thus will be highly relevant to mineral exploration in Australia and offshore.Read moreRead less