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Research Topic : structural interview
Socio-Economic Objective : Other
Field of Research : Geology
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  • Researchers (21)
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  • Funded Activity

    Discovery Projects - Grant ID: DP0346828

    Funder
    Australian Research Council
    Funding Amount
    $270,000.00
    Summary
    A Direct Approach to Crystal Structure Determination - a solution to the phase problem. The purpose of this research is to determine the positions of atoms in crystals and nano-crystals. We have developed a theory that shows how to extract all of the information required to determine atomic positions from such crystals and we have carried through initial successful tests on simple materials. In particular, we have found that crystallographic phase, hitherto not directly measurable, can in fact b .... A Direct Approach to Crystal Structure Determination - a solution to the phase problem. The purpose of this research is to determine the positions of atoms in crystals and nano-crystals. We have developed a theory that shows how to extract all of the information required to determine atomic positions from such crystals and we have carried through initial successful tests on simple materials. In particular, we have found that crystallographic phase, hitherto not directly measurable, can in fact be extracted uniquely from a single electron diffraction pattern. This constitutes a solution to the phase problem in crystallography. It is now our aim to develop this method into a routine technique.
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    Funded Activity

    Discovery Projects - Grant ID: DP0345310

    Funder
    Australian Research Council
    Funding Amount
    $162,000.00
    Summary
    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.
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    Funded Activity

    Discovery Projects - Grant ID: DP0211890

    Funder
    Australian Research Council
    Funding Amount
    $227,718.00
    Summary
    MACQUARIE ISLAND: A UNIQUE WINDOW INTO THE OCEAN BASEMENT AND THE LINK BETWEEN OCEAN RIDGES AND OPHIOLITES. Knowledge about the composition and structure of the oceanic crust is limited due to the inaccessibility of the deep-ocean floor. Macquarie Island is the only fragment of ocean crust and mantle exposed above sea-level in the world, providing a unique opportunity to study processes of oceanic floor generation in-situ. Our project will carry out detailed mapping of the lower crust and mantle .... MACQUARIE ISLAND: A UNIQUE WINDOW INTO THE OCEAN BASEMENT AND THE LINK BETWEEN OCEAN RIDGES AND OPHIOLITES. Knowledge about the composition and structure of the oceanic crust is limited due to the inaccessibility of the deep-ocean floor. Macquarie Island is the only fragment of ocean crust and mantle exposed above sea-level in the world, providing a unique opportunity to study processes of oceanic floor generation in-situ. Our project will carry out detailed mapping of the lower crust and mantle sections on the island, followed by an integrated microstructural, petrological, and geochronological analysis of samples. Such investigations may lead to fundamental advances in the understanding of formation, deformation, and emplacement of oceanic crust at mid-ocean ridge spreading centres.
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    Funded Activity

    Discovery Projects - Grant ID: DP0773097

    Funder
    Australian Research Council
    Funding Amount
    $315,000.00
    Summary
    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.
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    Funded Activity

    Linkage Projects - Grant ID: LP0560887

    Funder
    Australian Research Council
    Funding Amount
    $420,000.00
    Summary
    Deciphering the tectonic history of the Musgrave Block to assist mineral explorers and regional synthesis programs. Effective mineral exploration strategies in complex basement terrains are increasingly reliant on integrated, data-rich, tectonic models. In this project we will focus a large multidisciplinary team to develop a tectonic model for the evolution of the Musgrave Block in central Australia. This large, poorly understood terrain occupies a critical structural location, separating the .... Deciphering the tectonic history of the Musgrave Block to assist mineral explorers and regional synthesis programs. Effective mineral exploration strategies in complex basement terrains are increasingly reliant on integrated, data-rich, tectonic models. In this project we will focus a large multidisciplinary team to develop a tectonic model for the evolution of the Musgrave Block in central Australia. This large, poorly understood terrain occupies a critical structural location, separating the northern and southern Australian cratons. By constraining models of crustal evolution and architecture, the project will underpin future mineral exploration programs in this highly prospective greenfields region and define the role of the Musgrave Block in the assembly of Proterozoic Australia.
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    Funded Activity

    Linkage Projects - Grant ID: LP0454301

    Funder
    Australian Research Council
    Funding Amount
    $576,444.00
    Summary
    Developing a Tectonic Framework for the Gawler Craton: Paving the Way for Successful Mineral Exploration Programs. The late Archaean to Mesoproterozoic Gawler Craton is the major Precambrian province in southern Australia. However, despite containing one of the largest orebodies on Earth, exploration expenditure in the craton has been comparatively low, and hampered by insufficient knowledge of the craton's tectonic systems. This project uses an integrated package of geochemical, isotopic and .... Developing a Tectonic Framework for the Gawler Craton: Paving the Way for Successful Mineral Exploration Programs. The late Archaean to Mesoproterozoic Gawler Craton is the major Precambrian province in southern Australia. However, despite containing one of the largest orebodies on Earth, exploration expenditure in the craton has been comparatively low, and hampered by insufficient knowledge of the craton's tectonic systems. This project uses an integrated package of geochemical, isotopic and geophysical tools to develop a comprehensive model for the tectonic evolution of the Gawler Craton. The project will constrain the development of the Gawler Craton in the context of Precambrian Australian evolution, and offer insights into universal processes of lithosphere formation, growth and stabilisation.
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    Funded Activity

    Discovery Projects - Grant ID: DP0344708

    Funder
    Australian Research Council
    Funding Amount
    $260,000.00
    Summary
    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.
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    Funded Activity

    Discovery Projects - Grant ID: DP0665094

    Funder
    Australian Research Council
    Funding Amount
    $295,000.00
    Summary
    Tectonic links between the Musgrave Province and the North Australian Craton: correlations, event chronology, and tectonothermal regimes. Developing effective mineral exploration strategies relies on data-rich tectonic models that seek to explain the full history of a terrain. In the Australian context the tectonic evolution of the Musgrave Province is a key focus of the minerals industry due to its widely recognised potential for base-metal mineralisation. This project will develop tectonic mod .... Tectonic links between the Musgrave Province and the North Australian Craton: correlations, event chronology, and tectonothermal regimes. Developing effective mineral exploration strategies relies on data-rich tectonic models that seek to explain the full history of a terrain. In the Australian context the tectonic evolution of the Musgrave Province is a key focus of the minerals industry due to its widely recognised potential for base-metal mineralisation. This project will develop tectonic models that encompass the evolution of the Musgrave Province and the adjacent North Australia Craton. The outcomes of the project will reduce risk to mineral explorers and make an important contribution to the broader question Australia's Proterozoic evolution.
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    Funded Activity

    Linkage Projects - Grant ID: LP0455621

    Funder
    Australian Research Council
    Funding Amount
    $81,518.00
    Summary
    Structural and hydrothermal fluid control of high-grade (>65 wt% Fe) hematite ores in BIF-hosted iron deposits in the Hamersley Basin. The project aims to understand the geological controls on high-grade(>65wt%Fe)iron ore deposits of the Hamersley Province. In particular, the role of hydrothermal fluids in the transformation of banded iron formation (BIF) to high-grade iron ore. Three deposits (Mt Tom Price, Paraburdoo and Channar) provide an ideal study of the relationship between the struct .... Structural and hydrothermal fluid control of high-grade (>65 wt% Fe) hematite ores in BIF-hosted iron deposits in the Hamersley Basin. The project aims to understand the geological controls on high-grade(>65wt%Fe)iron ore deposits of the Hamersley Province. In particular, the role of hydrothermal fluids in the transformation of banded iron formation (BIF) to high-grade iron ore. Three deposits (Mt Tom Price, Paraburdoo and Channar) provide an ideal study of the relationship between the structural evolution, timing, and characteristics of hydrothermal and supergene processes. In particular, the the study aims to investigate the structural control and fluid chemistry of the hydrothermal system. The outcomes of this study will include a better understanding about the timing and fluid characteristcs of hydrothermal/supergene events and their significance to the formation and geometry of high-grade iron ore deposits in the Hamersley Province.
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