Present-Day Crustal Stress Field of North-Eastern Australia. The key project benefit is to advance fundamental understanding of crustal dynamics in NE Australia and thus Australia as a whole. The project will improve our knowledge of both the nature and sources of the present-day crustal stresses in NE Australia. The project has implications for seismicity and neotectonics in NE Australia. Furthermore, the project has significant implications for both hydrocarbon and hot dry rock geothermal ener ....Present-Day Crustal Stress Field of North-Eastern Australia. The key project benefit is to advance fundamental understanding of crustal dynamics in NE Australia and thus Australia as a whole. The project will improve our knowledge of both the nature and sources of the present-day crustal stresses in NE Australia. The project has implications for seismicity and neotectonics in NE Australia. Furthermore, the project has significant implications for both hydrocarbon and hot dry rock geothermal energy exploration and development.Read moreRead less
The seismic signature of crustal fluids. Fluids are expected to profoundly modify the seismic properties of the cracked rocks of Earth's upper crust (to depths of about 15 km) but there are so far few relevant laboratory measurements. Through the development and application of novel experimental techniques we plan to build a better laboratory-based understanding of the seismic properties of fluid-saturated crustal rocks. The outcome will be an improved capacity to monitor the presence of fluid ....The seismic signature of crustal fluids. Fluids are expected to profoundly modify the seismic properties of the cracked rocks of Earth's upper crust (to depths of about 15 km) but there are so far few relevant laboratory measurements. Through the development and application of novel experimental techniques we plan to build a better laboratory-based understanding of the seismic properties of fluid-saturated crustal rocks. The outcome will be an improved capacity to monitor the presence of fluids in diverse situations ranging from geothermal power generation and waste disposal to earthquake fault zones. Read moreRead less
Present-Day Stress and Tectonics of Deltas and Deepwater Fold-Thrust Belts. The key benefit of the project will be to advance our understanding of the geological processes that control the development of deltas, and of the fold-thrust belts located in deepwater adjacent to deltas, by analysis of five examples worldwide. Global hydrocarbon exploration is successfully moving to deepwater fold-thrust belts. One of Australia's key under-explored frontier petroleum provinces is the Australian Bight B ....Present-Day Stress and Tectonics of Deltas and Deepwater Fold-Thrust Belts. The key benefit of the project will be to advance our understanding of the geological processes that control the development of deltas, and of the fold-thrust belts located in deepwater adjacent to deltas, by analysis of five examples worldwide. Global hydrocarbon exploration is successfully moving to deepwater fold-thrust belts. One of Australia's key under-explored frontier petroleum provinces is the Australian Bight Basin. The prospective parts of this basin comprise delta/deepwater fold-thrust belt systems and analysis of more data-rich systems worldwide will help provide the geological knowledge required to help re-invigorate exploration in the Bight Basin.Read moreRead less
Shear heating in granular materials: micromechanics of thermal conduction and production. Oil, gas and geothermal exploration are amongst the major energy industries in Australia and must be optimised to enable efficient production. These processes are dominated by the transfer of heat through granular soil media. Past research was based on continuum heat-flow solutions, but these problems are governed by distinct networks of particle-particle contacts and interparticle pore-fluids. Heat-flow so ....Shear heating in granular materials: micromechanics of thermal conduction and production. Oil, gas and geothermal exploration are amongst the major energy industries in Australia and must be optimised to enable efficient production. These processes are dominated by the transfer of heat through granular soil media. Past research was based on continuum heat-flow solutions, but these problems are governed by distinct networks of particle-particle contacts and interparticle pore-fluids. Heat-flow solutions depend on effective terms of thermal conduction, production and convection, but these change with loading. A systematic study must therefore be accomplished to formulate the micromechanics of the effective thermal properties, such that continuum solutions are refined to optimise energy exploration.Read moreRead less
Solidification, Channel Formation and Thermal Erosion In Lava Flows. This project will elucidate the complex dynamics that control the cooling rates and advance rates of lava flows. It will result in improved hazard assessments for volcanic areas around the world affected by the advance of lava flows, including many Pacific islands and most countries around the Pacific Rim. The project will also provide a quantitative understanding of thermal erosion in lava channels, which will help explain th ....Solidification, Channel Formation and Thermal Erosion In Lava Flows. This project will elucidate the complex dynamics that control the cooling rates and advance rates of lava flows. It will result in improved hazard assessments for volcanic areas around the world affected by the advance of lava flows, including many Pacific islands and most countries around the Pacific Rim. The project will also provide a quantitative understanding of thermal erosion in lava channels, which will help explain the formation and location of major ore deposits of nickel, copper and platinum in Western Australia and elsewhere around the world.Read moreRead less
NUMERICAL MODELS OF PLATE TECTONICS, MANTLE CONVECTION AND SLAB DYNAMICS WITH EVOLVING FAULTS. We plan to develop a method for simulating large-scale
geological structures with a much improved treatment
of tectonic faults in 3D.
Current computer models have sharp geological faults at plate
boundaries represented by broad, blurred zones. New techniques
for modeling cracks in engineering structures will be scaled up to
the whole Earth.
This will help us to understand how the Earth's p ....NUMERICAL MODELS OF PLATE TECTONICS, MANTLE CONVECTION AND SLAB DYNAMICS WITH EVOLVING FAULTS. We plan to develop a method for simulating large-scale
geological structures with a much improved treatment
of tectonic faults in 3D.
Current computer models have sharp geological faults at plate
boundaries represented by broad, blurred zones. New techniques
for modeling cracks in engineering structures will be scaled up to
the whole Earth.
This will help us to understand how the Earth's plates move and
interact now and in the past and how the structure of the continents
arose.
Not only is this intrinsically interesting, it
will also be of immediate practical benefit to geological modelers.Read moreRead less
Mineral Physics of the Earth's Core. Most information on the nature of Earth's core properties has come from teleseismic studies, which detect weak earthquake-wave signals that have traversed the Earth's deepest interior. These studies have revealed several unusual and enigmatic phenomena in the core, but interpretation of these observations must rely on mineral-physics data on the materials of the core (e.g. iron-based alloys). This project will create a unique world-class ultra-high pressure l ....Mineral Physics of the Earth's Core. Most information on the nature of Earth's core properties has come from teleseismic studies, which detect weak earthquake-wave signals that have traversed the Earth's deepest interior. These studies have revealed several unusual and enigmatic phenomena in the core, but interpretation of these observations must rely on mineral-physics data on the materials of the core (e.g. iron-based alloys). This project will create a unique world-class ultra-high pressure laboratory to obtain such data. By defining the composition and mineralogy of Earth's core, it will place Australia in the forefront of this exciting research field, and will also represent a major national resource for the study of novel materials at extreme conditions.Read moreRead less
Proterozoic tectonic evolution of Australia and India. Recent studies cast doubt on reconstructions of the Neoproterozoic supercontinent Rodinia, and on the tectonic coherence of East Gondwanaland (Australia, Antarctica and India). Within Australia, the relative positions of the major crustal blocks during most of the Proterozoic era remain largely unverified. Fossil magnetism in rocks of different ages from the major crustal blocks of Australia and India will be used to determine whether the ....Proterozoic tectonic evolution of Australia and India. Recent studies cast doubt on reconstructions of the Neoproterozoic supercontinent Rodinia, and on the tectonic coherence of East Gondwanaland (Australia, Antarctica and India). Within Australia, the relative positions of the major crustal blocks during most of the Proterozoic era remain largely unverified. Fossil magnetism in rocks of different ages from the major crustal blocks of Australia and India will be used to determine whether the blocks were together or were separated by large oceans during Proterozoic time. The results will place fundamental constraints on the geological, palaeogeographic, and palaeobiological evolution of Australia, Rodinia, and the early Earth as a whole.Read moreRead less
Thermal structure and evolution of the Australian continent. Australia contains 40% of the world's known uranium resources. Uranium, with thorium and potassium, are heat-producing elements which affect the way temperature varies within the Earth. Outcomes from this project will lead to a better understanding of the potential for geothermal energy in Australia and provide a framework for assessing Australia's uranium resource. Understanding the crustal thermal regime is also fundamental to our kn ....Thermal structure and evolution of the Australian continent. Australia contains 40% of the world's known uranium resources. Uranium, with thorium and potassium, are heat-producing elements which affect the way temperature varies within the Earth. Outcomes from this project will lead to a better understanding of the potential for geothermal energy in Australia and provide a framework for assessing Australia's uranium resource. Understanding the crustal thermal regime is also fundamental to our knowledge of many earth processes. The project will enhance Australia's international research standing, provide training for an early career researcher and contribute to the development of an environmentally sustainable Australia, a National research priority.Read moreRead less
Coupled subduction dynamics and continent deformations: understanding the Asian and Red Sea tectonics. Modeling slab pull forces and lithospheric deformation provides a new insight in the dynamics of plate tectonics. Unraveling the self-consistent formation of faults, rifts, shear zones and up to passive margin will further the understanding of our planet. Furthermore the application of these models to specific geological contexts will support the exploration and assessment of inaccessible Ear ....Coupled subduction dynamics and continent deformations: understanding the Asian and Red Sea tectonics. Modeling slab pull forces and lithospheric deformation provides a new insight in the dynamics of plate tectonics. Unraveling the self-consistent formation of faults, rifts, shear zones and up to passive margin will further the understanding of our planet. Furthermore the application of these models to specific geological contexts will support the exploration and assessment of inaccessible Earth's resources, such as hydrocarbons pools, located along the deep Australian continent margins, and diamonds and ore deposits, associated with continental shear zones, which potential is still to be fully discovered.Read moreRead less