Investigating mineral alteration and infilling of discontinuities in naturally deformed rocks as a guide to rock mass rheology. Structural analysis of naturally deformed rock will be used to investigate the origin, physical characteristics and frictional behaviour of naturally formed discontinuity surfaces. Discontinuities in naturally deformed rock masses are typically altered and infilled with complex combinations of mineral matter and are a major control on the rheology, including strength a ....Investigating mineral alteration and infilling of discontinuities in naturally deformed rocks as a guide to rock mass rheology. Structural analysis of naturally deformed rock will be used to investigate the origin, physical characteristics and frictional behaviour of naturally formed discontinuity surfaces. Discontinuities in naturally deformed rock masses are typically altered and infilled with complex combinations of mineral matter and are a major control on the rheology, including strength and stability, of rock masses in engineering excavations. By combining structural geology techniques and laboratory experiments, and with reference to existing data on field-scale rock mass deformation derived from engineering rock mechanics investigations, a methodology for predicting rock mass rheology from fundamental geological observations will be devised and tested.Read moreRead less
The ins and outs of a Proterozoic supercontinent - what is the significance of 990-900 Ma orogenesis for the assembly of Rodinia? The hypothesis that all of Earth's continents came together one billion years ago to form a supercontinent known as Rodinia has invigorated debate about ancient continental distributions. Current models depict a flawed configuration for Rodinia, since they assume that continental fragments preserving evidence for quite different episodes of tectonic activity between ....The ins and outs of a Proterozoic supercontinent - what is the significance of 990-900 Ma orogenesis for the assembly of Rodinia? The hypothesis that all of Earth's continents came together one billion years ago to form a supercontinent known as Rodinia has invigorated debate about ancient continental distributions. Current models depict a flawed configuration for Rodinia, since they assume that continental fragments preserving evidence for quite different episodes of tectonic activity between 1350 and 900 million years ago developed at the same time. This project will make new correlations based upon careful observation and precise isotopic dating of rocks in Antarctica and Mexico, and will use these data to develop a more realistic picture of the ancient Earth.Read moreRead less
Geodynamic evolution of the Banda Arc. The project will contribute to a better understanding of plate tectonic processes and will provide insights into the dynamics of the Indo-Australian plate. This information is fundamentally important for estimating seismic hazards and the potential for generating large magnitude earthquakes in Australia. Outcomes of this project will facilitate to unravel analogue tectonic systems that were active during the geological evolution of Australia (e.g. the Lachl ....Geodynamic evolution of the Banda Arc. The project will contribute to a better understanding of plate tectonic processes and will provide insights into the dynamics of the Indo-Australian plate. This information is fundamentally important for estimating seismic hazards and the potential for generating large magnitude earthquakes in Australia. Outcomes of this project will facilitate to unravel analogue tectonic systems that were active during the geological evolution of Australia (e.g. the Lachlan fold belt in eastern Australia), thus providing a new insight into the Australian environment. The project will also elucidate the nature of tectonic processes that are known to generate major ore deposits and is therefore likely to have important economic implications.Read moreRead less
Microscale evolution of deformed rocks and glaciers. Scientific outcomes from this research have significant implications for predictions on material properties and are applicable to rock behaviour in mineralised systems, a focus of Australia's minerals industry, and the development of new materials for the Australian manufacturing industries. It will help maintain Australia's excellent international research reputation in the fields of microstructural geology and glaciology.
Microstructural analysis using integrated experiments and numerical modelling. Microstructures related to nano-materials and visible up to the scale of a thin section, are important tools for any material scientist, geologist or glaciologist. Microstructural evolution underpins how these disciplines unravel grain-scale structures, deformation conditions and mechanisms to estimate the intensity or amount of deformation. This project will allow us to better interpret microstructural evolution, in ....Microstructural analysis using integrated experiments and numerical modelling. Microstructures related to nano-materials and visible up to the scale of a thin section, are important tools for any material scientist, geologist or glaciologist. Microstructural evolution underpins how these disciplines unravel grain-scale structures, deformation conditions and mechanisms to estimate the intensity or amount of deformation. This project will allow us to better interpret microstructural evolution, in a range of natural, organic and composite materials, by using integrated laboratory experiments and numerical simulations. With these results we will model the conditions that prevail in composite materials, in glaciers and apply them to processes operating in of the Earth's crust.Read moreRead less
The eruption, emplacement and characteristics of extremely large volume pyroclastic flow deposits (ignimbrites). Pyroclastic flows are hot, turbulent, flows of volcanic gas, pumice, rock debris and fine ash often produced during major explosive volcanic eruptions. Most historic and researched events have been mostly small volume examples. In this research we propose to investigate the characteristics of 3 extremely large volume (>1,000 km3) pyroclastic flow deposits in the Andes of South America ....The eruption, emplacement and characteristics of extremely large volume pyroclastic flow deposits (ignimbrites). Pyroclastic flows are hot, turbulent, flows of volcanic gas, pumice, rock debris and fine ash often produced during major explosive volcanic eruptions. Most historic and researched events have been mostly small volume examples. In this research we propose to investigate the characteristics of 3 extremely large volume (>1,000 km3) pyroclastic flow deposits in the Andes of South America, to understand the eruption origins and the flow dynamics of such large volume and potentially far flowing (up to 200 km from the vent) pyroclastic flows. These are potentially more destructive than the Indian Ocean tsunami event, and eruptions of this magnitude could occur in Indonesia, PNG and New Zealand.Read moreRead less
Neotectonics of the Indo-Australian plate. This project will contribute fundamental insights into the dynamics of our planet, towards earthquake risk assessment and to evolution of Australia's distinctive landscapes. The benefit of this project can therefore be evaluated in light of its contribution to the social and economic repercussions of improved understanding of earthquake risk and our landscapes and our place in them.
Obduction, lithospheric flexure and basin formation. The proposal aims to investigate the links between hydrocarbon basins and obduction, or emplacement of oceanic crust onto continental margins. Obduction of the Samail Ophiolite of Oman onto the Arabian Peninsular at a time of the world's largest hydrocarbon accumulation, requires a causative relationship. This event remains poorly constrained and controversial, and therefore limits exploration models for hydrocarbons. Understanding the dynamic ....Obduction, lithospheric flexure and basin formation. The proposal aims to investigate the links between hydrocarbon basins and obduction, or emplacement of oceanic crust onto continental margins. Obduction of the Samail Ophiolite of Oman onto the Arabian Peninsular at a time of the world's largest hydrocarbon accumulation, requires a causative relationship. This event remains poorly constrained and controversial, and therefore limits exploration models for hydrocarbons. Understanding the dynamics of obduction of ocean crust onto a passive continental margin and the resultant flexural basin is of major global importance. This proposal addresses this issue in the superbly exposed Arabian Pensinsular, applying geochronology, basin analysis and basin modelling techniques.Read moreRead less
Quantifying the Phanerozoic thermal evolution and long-term stability of cratonic lithosphere using integrated low temperature thermochronology. The Earth's most ancient crustal regions (i.e. cratons) are thought to have remained remarkably stable since their formation >2.5 billion years ago. This project will re-evaluate this paradigm by applying low temperature thermochronology by the fission track and (U-Th)/He methods to three key cratons, to detect and quantify previously unknown episodes o ....Quantifying the Phanerozoic thermal evolution and long-term stability of cratonic lithosphere using integrated low temperature thermochronology. The Earth's most ancient crustal regions (i.e. cratons) are thought to have remained remarkably stable since their formation >2.5 billion years ago. This project will re-evaluate this paradigm by applying low temperature thermochronology by the fission track and (U-Th)/He methods to three key cratons, to detect and quantify previously unknown episodes of significant cooling and denudation (i.e. low-level instability) which are invisible to other analytical techniques. The outcomes will open a new research avenue in these terrains, which host some of the world's most valuable mineral resources, underlie important petroleum basins and are potential long-term repositories for radioactive waste. Read moreRead less
Argon thermochronometers and the effects of recrystallization. Rocks exhumed from high temperatures in continental settings contain a record of cooling in potassium-bearing minerals, known as thermochronometers, due to the quantitative retention of radiogenic argon below some characteristic closure temperature. However, thermochronometers may be affected by recrystallization processes occurring below such temperatures, and in some cases argon data record the timing of crystallization rather tha ....Argon thermochronometers and the effects of recrystallization. Rocks exhumed from high temperatures in continental settings contain a record of cooling in potassium-bearing minerals, known as thermochronometers, due to the quantitative retention of radiogenic argon below some characteristic closure temperature. However, thermochronometers may be affected by recrystallization processes occurring below such temperatures, and in some cases argon data record the timing of crystallization rather than cooling. Field, microstructural and isotopic analysis will be used to evaluate the effects of recrystallization on the muscovite and potassium-feldspar thermochronometers, particularly in fault zones. Understanding the effects of recrystallization on thermochronometers is critical for studies of the assembly of the continental crust.Read moreRead less