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Australian State/Territory : TAS
Socio-Economic Objective : Other
Field of Research : Geology
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  • Funded Activity

    Linkage Projects - Grant ID: LP0668018

    Funder
    Australian Research Council
    Funding Amount
    $73,950.00
    Summary
    Genesis of platinum group element-rich, unconformity-style, hydrothermal mineral deposits, as inferred from a Northern Territory example. Mineral products currently provide a great deal of Australia's exports to international markets, and underpin much of our economy. However, Australia can only maintain this position through continued improvement of mineral discovery rates, particularly for high value, deep earth resources. This project aims to improve the likelihood of the discovery of higher .... Genesis of platinum group element-rich, unconformity-style, hydrothermal mineral deposits, as inferred from a Northern Territory example. Mineral products currently provide a great deal of Australia's exports to international markets, and underpin much of our economy. However, Australia can only maintain this position through continued improvement of mineral discovery rates, particularly for high value, deep earth resources. This project aims to improve the likelihood of the discovery of higher value hydrothermal orebodies. This will improve the value of mineral exports, raise exploration levels in some Australian provinces (thus stimulating economic activity in regional and industrial sectors), and help invigorate training within the geoscience arm of the university sector.
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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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    Funded Activity

    Linkage Projects - Grant ID: LP0453794

    Funder
    Australian Research Council
    Funding Amount
    $270,000.00
    Summary
    Geochronology, Metallogenesis and Deposit Styles of Loei Foldbelt in Thailand and Laos PDR. The Loei volcanic-plutonic belt occurs in Thailand and Laos PDR between two major crustal terranes in mainland SE Asia: Shan-Thai in the west and Indochina terrane in the east. Several skarn type copper-gold and porphyry related epithermal gold deposits are distributed along the Loei belt, and yet these deposits are not well documented in the literature. Detailed metallogenic relations and evolution of th .... Geochronology, Metallogenesis and Deposit Styles of Loei Foldbelt in Thailand and Laos PDR. The Loei volcanic-plutonic belt occurs in Thailand and Laos PDR between two major crustal terranes in mainland SE Asia: Shan-Thai in the west and Indochina terrane in the east. Several skarn type copper-gold and porphyry related epithermal gold deposits are distributed along the Loei belt, and yet these deposits are not well documented in the literature. Detailed metallogenic relations and evolution of these mineral deposits are also poorly understood; it is not known whether they formed from single, long-lived intrusive-centred mineralised systems or multiple/episodic mineralised systems. Understanding the geotectonic and metallogenic relations of this belt have a direct benefit to Australian companies exploring in SE Asia, and the research results also can be applied back in Australia for exploration of Cu-Au deposits.
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