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.Read moreRead less
Driving Mechanisms of Mountain Building in Accretionary Orogens. Accretionary mountain belts constitute major portions of the Earth's continental crust including the Yilgarn in Western Australia and the area east of Broken Hill constituting a third of the Australian land mass. Understanding the origin of the Permo-Triassic (300-230 Ma) mountain range that lay along the margin of Gondwana from Eastern Australia to South America will provide a new insight into our environment and stimulate interna ....Driving Mechanisms of Mountain Building in Accretionary Orogens. Accretionary mountain belts constitute major portions of the Earth's continental crust including the Yilgarn in Western Australia and the area east of Broken Hill constituting a third of the Australian land mass. Understanding the origin of the Permo-Triassic (300-230 Ma) mountain range that lay along the margin of Gondwana from Eastern Australia to South America will provide a new insight into our environment and stimulate international interest through collaboration amongst researchers around the world. Accretionary orogens are of economic importance as they host the Earth's major orogenic gold deposits and our work has potential to provide a new framework for linking mineralization and deformation events within these important settings.Read moreRead less
Geological controls on high-grade oreshoots in the Wallaby gold deposit, Western Australia: Understanding the role of magmatic fluids in an Orogenic Au system. This project aims to understand the geological controls on high-grade (>2 g/t Au) oreshoots at the world-class Wallaby gold deposit (>7 Moz Au). In particular, the role of magmatic fluids in the transport and deposition of gold will be investigated. The Wallaby gold deposit is an ideal natural laboratory to investigate the complex relatio ....Geological controls on high-grade oreshoots in the Wallaby gold deposit, Western Australia: Understanding the role of magmatic fluids in an Orogenic Au system. This project aims to understand the geological controls on high-grade (>2 g/t Au) oreshoots at the world-class Wallaby gold deposit (>7 Moz Au). In particular, the role of magmatic fluids in the transport and deposition of gold will be investigated. The Wallaby gold deposit is an ideal natural laboratory to investigate the complex relationship between the geometry and timing of faults, influx of multiple hydrothermal fluid events and the deposition of gold. In particular, the study will investigate the relative importance of intrusion-related, and fault zone-related events in the formation of high-grade ore shoots. The outcomes of this study will include a clear understanding about the timing and relative contribution of magmatic and fault zone related events and their significance to the formation and geometry of high-grade oreshoots.Read moreRead less
Tectonic evolution and lode gold mineralisation in the Southern Cross district, Yilgarn Craton (Western Australia): a study of the meso- to Neoarchaean missing link. In the December quarter 2008, Gold export earnings increased by 2 per cent to $3.9 billion. Over the past 20 years and despite an increase in exploration expenditure to around $50 million per year, the discovery rates have been declining. Although the easy targets have been found, there remains considerable potential for future ma ....Tectonic evolution and lode gold mineralisation in the Southern Cross district, Yilgarn Craton (Western Australia): a study of the meso- to Neoarchaean missing link. In the December quarter 2008, Gold export earnings increased by 2 per cent to $3.9 billion. Over the past 20 years and despite an increase in exploration expenditure to around $50 million per year, the discovery rates have been declining. Although the easy targets have been found, there remains considerable potential for future major discoveries. This project addresses the pressing need for new data and improved exploration techniques to enable industry to target new discoveries. As the Southern Cross district is located in remote communities such discoveries also have major benefits for regional Australia.Read moreRead less
The Early Stages of Granite Evolution: Extraction and Transport Through Ductile Crust . This research is aimed at understanding how the continents develop through several stages of rock melting. Rock melts deep in the continents to form granite magmas which rise, transporting to the upper crust important metals, such as gold, copper and tin, and heat producing elements such as uranium, thorium and potassium. This research proposal seeks to understand how granite melts form and rise transporting ....The Early Stages of Granite Evolution: Extraction and Transport Through Ductile Crust . This research is aimed at understanding how the continents develop through several stages of rock melting. Rock melts deep in the continents to form granite magmas which rise, transporting to the upper crust important metals, such as gold, copper and tin, and heat producing elements such as uranium, thorium and potassium. This research proposal seeks to understand how granite melts form and rise transporting these all important elements, which control not only our wealth but also the stability of the continents we live in.Read moreRead less
Defining the multi-scale controls on high-grade gold mineralisation. This project aims to improve our understanding of how extremely high-grade gold occurrences form in order to further our understanding of metal transport and accumulation within the Earth’s crust. This project will generate new knowledge in the area of gold geochemistry using novel experimental programs, interdisciplinary approaches and by utilising advanced technologies. Expected outcomes of this project include reducing the ....Defining the multi-scale controls on high-grade gold mineralisation. This project aims to improve our understanding of how extremely high-grade gold occurrences form in order to further our understanding of metal transport and accumulation within the Earth’s crust. This project will generate new knowledge in the area of gold geochemistry using novel experimental programs, interdisciplinary approaches and by utilising advanced technologies. Expected outcomes of this project include reducing the unpredictability of high-grade gold occurrences that impact both production and exploration strategies. This project should benefit the mineral industry partners by helping to discover high grade gold resources which is of great benefit to Australia.Read moreRead less