Modeling fluid flow and mineralisation at crustal interfaces. Several types of mineral resources, including some uranium, iron, and base metal ore deposits, may be created by fluid flow through and around interfaces in the Earth's crust. By understanding how, where and why such deposits form, we will assist exploration for future resources of these metals. Insights will also be gained into petroleum resource generation and extraction, the distribution of seismicity and volcanoes in time and spac ....Modeling fluid flow and mineralisation at crustal interfaces. Several types of mineral resources, including some uranium, iron, and base metal ore deposits, may be created by fluid flow through and around interfaces in the Earth's crust. By understanding how, where and why such deposits form, we will assist exploration for future resources of these metals. Insights will also be gained into petroleum resource generation and extraction, the distribution of seismicity and volcanoes in time and space, the problems of underground nuclear waste disposal and sequestration of CO2, and the potential for geothermal energy, with benefits in resource identification and/or hazard assessment in these areas.Read moreRead less
Fluid mixing in hydrothermal systems. Mixing of fluids within permeable rocks can cause significant chemical changes to the fluids and the rocks, for example it causes metals to be dissolved and transported. Accumulation into mineral deposits requires concentration mechanisms which are uncertain due to difficulty of detecting ancient fluid pathways. We will analyse these ancient fluids using new microanalytical and other combined techniques, thereby testing the role of fluid mixing as a mechanis ....Fluid mixing in hydrothermal systems. Mixing of fluids within permeable rocks can cause significant chemical changes to the fluids and the rocks, for example it causes metals to be dissolved and transported. Accumulation into mineral deposits requires concentration mechanisms which are uncertain due to difficulty of detecting ancient fluid pathways. We will analyse these ancient fluids using new microanalytical and other combined techniques, thereby testing the role of fluid mixing as a mechanism for efficient metal precipitation. The research has significance for exploration and models for mineral deposits, and for characterising other geological fluids, and provides opportunity for technical breakthroughs in microanalysis of fluid inclusions.Read moreRead less
Four dimensional lithospheric evolution and controls on mineral system distribution in Neoarchean to Paleoproterozoic terranes. This project will resolve important questions about the links between the evolution and preservation of continents and important mineral deposits in Australia and West Africa between 2.7 and 1.8 billion years ago. The results will improve the understanding of a key period of Earth history and make a major contribution to mineral exploration.