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Field of Research : Tectonics
Research Topic : GAS EXCHANGE
Field of Research : Structural Geology
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  • Researchers (22)
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  • Funded Activity

    Discovery Projects - Grant ID: DP120101460

    Funder
    Australian Research Council
    Funding Amount
    $260,000.00
    Summary
    Detachments in evaporites and shales: their controls on fold-thrust belt style and wedge geometry. Deepwater fold-thrust belts comprise large structural traps, currently a major focus of Australian petroleum exploration. The structural style of a fold-thrust belt is controlled by its detachment and new field analogues will demonstrate the fundamental role of detachments.
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    Funded Activity

    Linkage Infrastructure, Equipment And Facilities - Grant ID: LE120100061

    Funder
    Australian Research Council
    Funding Amount
    $285,000.00
    Summary
    A new seismic facility for investigating tectonic collision zones, earthquake hazards and passive imaging techniques. A new seismic facility will enable collaboration with overseas partners to better understand plate margin tectonics and earthquake hazard in our region for mutual benefit. It will also be used in pilot studies of areas endowed with deep earth resources, and in assessing regions of heightened earthquake activity in Australia.
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    Active Funded Activity

    Discovery Projects - Grant ID: DP160101158

    Funder
    Australian Research Council
    Funding Amount
    $230,000.00
    Summary
    Subsurface fluid flow through fractures in sedimentary basins. This project aims to improve understanding of subsurface fluid transport through fractures. Fractures in rock provide interconnected, hydraulically conductive networks enabling large-volume fluid transport through sedimentary basins. The ability of a fracture to transmit fluid is primarily controlled by the in situ stress field, but also by rock strength, fracture plane orientation and roughness and pore-fluid pressure. We have a goo .... Subsurface fluid flow through fractures in sedimentary basins. This project aims to improve understanding of subsurface fluid transport through fractures. Fractures in rock provide interconnected, hydraulically conductive networks enabling large-volume fluid transport through sedimentary basins. The ability of a fracture to transmit fluid is primarily controlled by the in situ stress field, but also by rock strength, fracture plane orientation and roughness and pore-fluid pressure. We have a good understanding of in situ stress within many sedimentary basins, but know very little about the nature and origin of natural fractures. This project aims to provide a detailed, quantitative understanding of the nature and origin of natural fractures in the subsurface, which is critical for predicting fluid migration within aquifers, carbon dioxide storage sites, and geothermal and hydrocarbon reservoirs.
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    Showing 1-3 of 3 Funded Activites

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