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Australian State/Territory : TAS
Field of Research : Sedimentology
Research Topic : COPPER
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  • Funded Activity

    Discovery Projects - Grant ID: DP150102578

    Funder
    Australian Research Council
    Funding Amount
    $481,100.00
    Summary
    Pyrite: a deep-time capsule of ocean chemistry and atmosphere oxidation. Surprisingly little is known about trace element trends in past oceans, even though these data are vital for interpreting the evolution of the Earth's atmosphere, evolutionary pathways of marine life and cycles of major mineral deposits. Using laser-based analysis of sedimentary pyrite in deep marine rocks, this project aims to produce, for the first time, temporal variation curves for 25 trace elements in seawater over the .... Pyrite: a deep-time capsule of ocean chemistry and atmosphere oxidation. Surprisingly little is known about trace element trends in past oceans, even though these data are vital for interpreting the evolution of the Earth's atmosphere, evolutionary pathways of marine life and cycles of major mineral deposits. Using laser-based analysis of sedimentary pyrite in deep marine rocks, this project aims to produce, for the first time, temporal variation curves for 25 trace elements in seawater over the last 3.5 billion years. Preliminary research has validated the technique and demonstrated major changes in certain trace elements over geologically short periods. Outcomes will assist the minerals industry in the discovery of new deposits of zinc, copper, gold and iron ore in Australia.
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    Funded Activity

    Discovery Projects - Grant ID: DP0449756

    Funder
    Australian Research Council
    Funding Amount
    $460,000.00
    Summary
    Submarine explosive eruptions of silicic magma: constraints on products and processes from modern sea-floor examples, ancient successions and experiments. Volcanoes are common on the sea-floor. Many have been the sites of devastating explosive eruptions throughout Earth history, producing thick layers of pumice and volcanic ash in both modern and ancient ocean basins. None of these events has been witnessed, hence, little is known about submarine explosive eruptions and the associated volcanoes. .... Submarine explosive eruptions of silicic magma: constraints on products and processes from modern sea-floor examples, ancient successions and experiments. Volcanoes are common on the sea-floor. Many have been the sites of devastating explosive eruptions throughout Earth history, producing thick layers of pumice and volcanic ash in both modern and ancient ocean basins. None of these events has been witnessed, hence, little is known about submarine explosive eruptions and the associated volcanoes. This detailed, multidisciplinary study will link exploration of modern explosive sea-floor volcanoes (western Pacific Ocean), field-work on older, submarine volcanic formations (Japan, Greece) and experiments that simulate explosive eruptions and their products. The results will elucidate sea-floor explosive volcanism and its contribution to the geology of ocean basins.
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    Active Funded Activity

    Linkage Projects - Grant ID: LP190100035

    Funder
    Australian Research Council
    Funding Amount
    $499,824.00
    Summary
    Exploration targeting from next-generation volcanic facies reconstruction. The project aims to develop new innovative image analysis techniques to reconstruct the architecture of the volcanic host at four highly prospective hydrothermal-magmatic ore deposits, and investigate the properties of rocks that favour high-grade ore mineralisation. Expected outcomes of this project include next-generation automated techniques for volcanic facies analysis, and predictions of where hydrothermal alteration .... Exploration targeting from next-generation volcanic facies reconstruction. The project aims to develop new innovative image analysis techniques to reconstruct the architecture of the volcanic host at four highly prospective hydrothermal-magmatic ore deposits, and investigate the properties of rocks that favour high-grade ore mineralisation. Expected outcomes of this project include next-generation automated techniques for volcanic facies analysis, and predictions of where hydrothermal alteration is most prospective for mineralisation. Both outcomes are relevant to the discovery of volcanic-hosted mineralisation globally. This project will provide significant benefit to the Australian mining industry by diversifying ore exploration strategies in the Australian crust, and will train the next generation of explorers.
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