Industrial Transformation Research Hubs - Grant ID: IH130200012
Funder
Australian Research Council
Funding Amount
$2,748,358.00
Summary
ARC Research Hub for Basin GEodyNamics and Evolution of SedImentary Systems (GENESIS). ARC Research Hub for Basin GEodyNamics and Evolution of SedImentary Systems (GENESIS). This Research Hub aims to undertake simultaneous modelling of deep Earth and surface processes, spanning basin scales to individual sediment grains. The Hub will develop and apply cutting-edge basin simulation approaches to transform the seeding and testing of basin exploration models, extending their viability to complex, ....ARC Research Hub for Basin GEodyNamics and Evolution of SedImentary Systems (GENESIS). ARC Research Hub for Basin GEodyNamics and Evolution of SedImentary Systems (GENESIS). This Research Hub aims to undertake simultaneous modelling of deep Earth and surface processes, spanning basin scales to individual sediment grains. The Hub will develop and apply cutting-edge basin simulation approaches to transform the seeding and testing of basin exploration models, extending their viability to complex, inaccessible remote and deep exploration targets. The Hub will fuse multidimensional data into five dimensional basin models (space and time, with uncertainty estimates) by coupling the evolution of mantle flow, crustal deformation, erosion and sedimentary processes, achieving a quantum leap in basin modelling and petroleum systems analysis.Read moreRead less
ARC Centre of Excellence for Core to Crust Fluid Systems. Water is essential for human existence, indeed for life's beginning. The circulation of water between the surface and the deep interior lubricates the internal dynamics that keep Earth geologically alive; it is crucial to most Earth systems, including the evolution of the hydrospher/atmosphere/biosphere, and the development of giant ore deposits. However, the origin, abundance, speciation and movements of fluids inside Earth are largely u ....ARC Centre of Excellence for Core to Crust Fluid Systems. Water is essential for human existence, indeed for life's beginning. The circulation of water between the surface and the deep interior lubricates the internal dynamics that keep Earth geologically alive; it is crucial to most Earth systems, including the evolution of the hydrospher/atmosphere/biosphere, and the development of giant ore deposits. However, the origin, abundance, speciation and movements of fluids inside Earth are largely unknown, and represent key issues in modern geoscience. This CoE will integrate previously disparate fields - geology, tectonics, geochemistry, petrophysics, geophysics and dynamic modelling - to understand the workings of Earth's deep plumbing system.Read moreRead less
Understanding the deep driving forces of Earth’s large-scale topography through time. We propose to model the convection of Earth’s mantle linked to tectonic plate motions to unravel their combined influence on the evolution of topography over 550 million years. The project will lead to an understanding of the driving forces of large-scale topography in continental interiors and along their margins through geological time.
The link between the deep Earth and its dynamic surface. Modelling the two-way interaction of plate tectonics with the actions of erosion and sedimentation gives a fundamentally new view of the dynamics of our planet and the importance of the surface on the deep interior. It will improve our understanding of the formation of sedimentary basins, their evolution and their preservation over geological time.
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.
Intraplate volcanism near lateral slab edges: result of deep mantle plumes or slab rollback-induced mantle flow? This project investigates how the Earth's interior (the mantle) flows near edges of tectonic plates as these plates sink into the mantle. This is important because these flows have been crucial in shaping the Southwest Pacific region bordering Australia and might be responsible for the formation of some of the largest volcanoes on Earth.
Indo-Australian Plate Active Tectonics Program. The Indo-Australian Plate Active Tectonics Program investigates fundamental questions in geodynamics using the unique record of landscape evolution in Australia. In this project the origin of iconic landscapes such as the Lake Eyre Basin and the Flinders Ranges will be addressed to explore the nature of the couplings between surface deformation and flow in the upper mantle, and between surface processes and tectonic activity.
Three-dimensional subduction models of overriding plate deformation and mantle flow using laboratory and numerical methods. This project investigates the interaction of the Earth's tectonic plates at subduction zones, places where one plate sinks below another plate into the Earth. This is important for understanding the evolution of the Australian plate that has active subduction zones to the north and east, and how its geological evolution is controlled by subduction.
Discovery Early Career Researcher Award - Grant ID: DE130100604
Funder
Australian Research Council
Funding Amount
$375,000.00
Summary
The dynamics of continent deformations. Modeling the coupling of subducting oceanic plates and deforming continents provides a fundamentally new view of the dynamics of our planet. It will improve an understanding of the formation of basins in continent interiors and their evolution over geological times.
Linkage Infrastructure, Equipment And Facilities - Grant ID: LE120100117
Funder
Australian Research Council
Funding Amount
$940,000.00
Summary
An advanced, macro-scale, hydro-thermo-mechanical testing chamber for sustainable deep geological applications. The Advanced Macro-scale Testing Chamber (AMTC) is a novel laboratory testing device capable of recreating deep geological conditions which can occur at depths of up to 13km underground. The AMTC will help scientists and engineers understand the Earth's behaviour during deep geological activities such as geothermal energy collection, pollutant disposal, underground mining and earthquak ....An advanced, macro-scale, hydro-thermo-mechanical testing chamber for sustainable deep geological applications. The Advanced Macro-scale Testing Chamber (AMTC) is a novel laboratory testing device capable of recreating deep geological conditions which can occur at depths of up to 13km underground. The AMTC will help scientists and engineers understand the Earth's behaviour during deep geological activities such as geothermal energy collection, pollutant disposal, underground mining and earthquake modelling.Read moreRead less