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Current Selection
Scheme : Discovery Projects
Field of Research : Geotectonics
Australian State/Territory : NSW
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Geotectonics (15)
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  • Researchers (9)
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  • Funded Activity

    Discovery Projects - Grant ID: DP0342933

    Funder
    Australian Research Council
    Funding Amount
    $360,000.00
    Summary
    From Synchrotron Characterisation of Single Fluid Inclusions to Archaean Geodynamics: An Integrated Study of Fluid-Rock Interaction in the Primitive Crust. In the primitive Earth, a wide range of phenomena including the initiation of biological activity and the formation of ore deposits were related to the mobilisation of mineralised fluids through the crust. In the Archaean craton of the Pilbara (WA), we have identified, within its tectonic framework, a crustal-scale plumbing system that channe .... From Synchrotron Characterisation of Single Fluid Inclusions to Archaean Geodynamics: An Integrated Study of Fluid-Rock Interaction in the Primitive Crust. In the primitive Earth, a wide range of phenomena including the initiation of biological activity and the formation of ore deposits were related to the mobilisation of mineralised fluids through the crust. In the Archaean craton of the Pilbara (WA), we have identified, within its tectonic framework, a crustal-scale plumbing system that channelled large volumes of mineralised hydrothermal solutions. Our objective is to understand the development of this plumbing system in relation to Archaean crustal geodynamics using a combination of structural geology, metamorphic petrology, geochronology, geochemistry, and the analysis of single-fluid inclusion using synchrotron and other X-ray sources.
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    Funded Activity

    Discovery Projects - Grant ID: DP0663373

    Funder
    Australian Research Council
    Funding Amount
    $195,000.00
    Summary
    Spreading ridge sedimentation processes: a novel approach using Macquarie Island as a natural laboratory. This research will examine the south eastern tectonic plate boundary of Australia, providing analogues for seafloor spreading related crustal processes that relate to present plate boundaries and ancient examples now joined to the Australian continent. The scientific innovation represented by this project will help Australian scientists to better understand an important part of the plate tec .... Spreading ridge sedimentation processes: a novel approach using Macquarie Island as a natural laboratory. This research will examine the south eastern tectonic plate boundary of Australia, providing analogues for seafloor spreading related crustal processes that relate to present plate boundaries and ancient examples now joined to the Australian continent. The scientific innovation represented by this project will help Australian scientists to better understand an important part of the plate tectonic cycle. This project will be of direct relevance to the Australian minerals exploration industry and will provide better constraints on rift-related metallogenesis.
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    Funded Activity

    Discovery Projects - Grant ID: DP0344841

    Funder
    Australian Research Council
    Funding Amount
    $60,000.00
    Summary
    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.
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    Funded Activity

    Discovery Projects - Grant ID: DP0770929

    Funder
    Australian Research Council
    Funding Amount
    $690,000.00
    Summary
    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.
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    Funded Activity

    Discovery Projects - Grant ID: DP0210311

    Funder
    Australian Research Council
    Funding Amount
    $1,355,000.00
    Summary
    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.
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    Funded Activity

    Discovery Projects - Grant ID: DP0984852

    Funder
    Australian Research Council
    Funding Amount
    $397,000.00
    Summary
    Diamond genesis: cracking the code for deep-Earth processes. The project will provide new insights into the processes by which diamond crystallises in the Earth's mantle, and will deliver information directly relevant to interpreting the diamond prospectivity of the Australian continent. The development of a new diamond mine in Australia, or by Australian companies abroad, would be a major addition to the economy and Australian-based industry. Another outcome of this research will be further de .... Diamond genesis: cracking the code for deep-Earth processes. The project will provide new insights into the processes by which diamond crystallises in the Earth's mantle, and will deliver information directly relevant to interpreting the diamond prospectivity of the Australian continent. The development of a new diamond mine in Australia, or by Australian companies abroad, would be a major addition to the economy and Australian-based industry. Another outcome of this research will be further development of methodologies for identification of sources of individual diamonds, relevant to the international Kimberley Process for reducing theft and illegal diamond trade. The project will be a highly visible Australian contribution to this global social and economic problem.
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    Funded Activity

    Discovery Projects - Grant ID: DP0344400

    Funder
    Australian Research Council
    Funding Amount
    $298,035.00
    Summary
    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.
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    Funded Activity

    Discovery Projects - Grant ID: DP0557326

    Funder
    Australian Research Council
    Funding Amount
    $240,000.00
    Summary
    Integrating Global Multidimensional Datasets to Underpin Subduction Process Modelling During the Past 60 Million Years. Subduction zones are the sites for massive sulphide, orogenic vein gold and porphyry deposits. As Australia derived 47% of it merchandise exports from its mineral and energy resources in 2001, ore-deposits constitute an important component of the Australian economy. Understanding the environment of subduction initiation and development as well as the signal that it imparts on .... Integrating Global Multidimensional Datasets to Underpin Subduction Process Modelling During the Past 60 Million Years. Subduction zones are the sites for massive sulphide, orogenic vein gold and porphyry deposits. As Australia derived 47% of it merchandise exports from its mineral and energy resources in 2001, ore-deposits constitute an important component of the Australian economy. Understanding the environment of subduction initiation and development as well as the signal that it imparts on the magmatic (ore-forming) arc, will provide improved efficiency for targeting Australia's deep-earth ore-deposits.
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    Funded Activity

    Discovery Projects - Grant ID: DP0556359

    Funder
    Australian Research Council
    Funding Amount
    $85,000.00
    Summary
    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.
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    Funded Activity

    Discovery Projects - Grant ID: DP0880801

    Funder
    Australian Research Council
    Funding Amount
    $337,999.00
    Summary
    The role of supercontinents in Earth's dynamic evolution. By better understanding the dynamic and volcanic evolution of continents, the project will contribute to our understanding of the long-term evolution and construction of the Australian plate, leading to better models for Australia's deep-Earth resources(NRP 1.6), and the impact of large-scale dynamics on ore-deposit formation. The geodynamic modelling capabilities implemented in this project will keep Australian at the cutting edge of Ge .... The role of supercontinents in Earth's dynamic evolution. By better understanding the dynamic and volcanic evolution of continents, the project will contribute to our understanding of the long-term evolution and construction of the Australian plate, leading to better models for Australia's deep-Earth resources(NRP 1.6), and the impact of large-scale dynamics on ore-deposit formation. The geodynamic modelling capabilities implemented in this project will keep Australian at the cutting edge of Geoinformatics (NRP 3.2). The project will strengthen ties between the mantle convection modelling and lithospheric dating communities, enhancing our understanding of complex Earth-system interactions, and promote international collaboration between Australia and the USA.
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