Physical and Chemical Constraints of Fluid Activated Processes During the Polyphase Tectonic Evolution of the Olary Domain, S.A. The Olary Domain, eastern South Australia, underwent several phases of deformation and metamorphism. These events mobilised fluids leading, amongst other features, to the formation of breccia bodies and mineral deposits. The complex nature of the geological evolution of the region obscures relationships of fluid migration to the structural history. Fluid inclusion stud ....Physical and Chemical Constraints of Fluid Activated Processes During the Polyphase Tectonic Evolution of the Olary Domain, S.A. The Olary Domain, eastern South Australia, underwent several phases of deformation and metamorphism. These events mobilised fluids leading, amongst other features, to the formation of breccia bodies and mineral deposits. The complex nature of the geological evolution of the region obscures relationships of fluid migration to the structural history. Fluid inclusion studies and stable isotope analyses combined with structural analyses on micro to macro scales shall establish links between the thermal and structural evolution of the area. This will provide insigth into the scale and physico-chemical characteristics of fluids and mineralising processes an relate these to the tectono-thermal history.Read moreRead less
In-situ solubility and speciation studies in super-critical H2O-NaCl-CO2 mixtures using synchrotron radiation. Understanding the physics and chemistry of metals in hypersaline and supercritical solutions represents a major scientific challenge with wide-ranging applications in the fields of mineral processing, economic geology, or CO2 sequestration. The advent of very bright sources of x-rays (synchrotrons) and development of spectroscopic cells that can contain corrosives samples at high pressu ....In-situ solubility and speciation studies in super-critical H2O-NaCl-CO2 mixtures using synchrotron radiation. Understanding the physics and chemistry of metals in hypersaline and supercritical solutions represents a major scientific challenge with wide-ranging applications in the fields of mineral processing, economic geology, or CO2 sequestration. The advent of very bright sources of x-rays (synchrotrons) and development of spectroscopic cells that can contain corrosives samples at high pressure and temperature allow for the first time the in-situ observation of these solutions. This project creates strong link between Australian and French scientists. By sharing the know-how developed at the European Synchrotron Research Facility, we aim to create a world-class facility at the Australian Synchrotron that will open in Melbourne in 2007.Read moreRead less
Transport of metals in vapours and brines: new insights into the formation of the Earth's mineral deposits. Traditional models for the formation of hydrothermal ore deposits assume that aqueous fluids transported the metals. This view is challenged by new observations showing that gold and copper are preferentially enriched in vapours coexisting with salty aqueous fluids in some deposits. This project uses state-of-the-art techniques and develops new instruments to measure experimentally the par ....Transport of metals in vapours and brines: new insights into the formation of the Earth's mineral deposits. Traditional models for the formation of hydrothermal ore deposits assume that aqueous fluids transported the metals. This view is challenged by new observations showing that gold and copper are preferentially enriched in vapours coexisting with salty aqueous fluids in some deposits. This project uses state-of-the-art techniques and develops new instruments to measure experimentally the partitioning of metals between solid, fluid and vapour at temperatures typical for natural ore deposits (350-550C, pressures varying for vapour saturated to 1 kb). By improving our understanding of metal transport within the Earth's crust, these data will lead to improved models and technologies for exploring and processing base and precious metals.Read moreRead less