Mapping Fluid Flow in the Earth's Crust: a Li and B micro-isotopic and thermodynamic study of serpentinisation. Interaction of fluids with magnesium-rich rocks creates new minerals and, on a global scale, affects the physical and chemical evolution of the Earth. On a more local scale, such fluid: rock interactions can lock up carbon dioxide via the formation of carbonate minerals. However, the extent to which such reactions may self-propagate is unclear. A primary benefit of this study will b ....Mapping Fluid Flow in the Earth's Crust: a Li and B micro-isotopic and thermodynamic study of serpentinisation. Interaction of fluids with magnesium-rich rocks creates new minerals and, on a global scale, affects the physical and chemical evolution of the Earth. On a more local scale, such fluid: rock interactions can lock up carbon dioxide via the formation of carbonate minerals. However, the extent to which such reactions may self-propagate is unclear. A primary benefit of this study will be new constraints on the viability of magnesium-rich rocks in geosequestration applications. Additional benefits will be provided by the development of advanced new analytical methodologies, and an increased level of understanding of the way that fluid flow can modify nickel sulphide ore bodies.Read moreRead less
A virtual exploration of iron-sulphur-world in search of the precursors to life on earth. The greenhouse gas, carbon dioxide, that currently presents a threat to the continued existence of humanity, ironically represents the starting point from which life on Earth probably originated. This research will probe the chemistry of how this gas, dissolved in ancient oceans, came to be converted to molecules that form the basis of living organisms through interaction with minerals, such as iron sulphid ....A virtual exploration of iron-sulphur-world in search of the precursors to life on earth. The greenhouse gas, carbon dioxide, that currently presents a threat to the continued existence of humanity, ironically represents the starting point from which life on Earth probably originated. This research will probe the chemistry of how this gas, dissolved in ancient oceans, came to be converted to molecules that form the basis of living organisms through interaction with minerals, such as iron sulphide. Aside from answering a fundamental question, it will offer insights into processes that convert a pollutant into a useful chemical, as well as what might happen if carbon dioxide is placed in mineral deposits for long-term storage.Read moreRead less