Pyrite: a deep-time capsule of ocean chemistry and atmosphere oxidation. Surprisingly little is known about trace element trends in past oceans, even though these data are vital for interpreting the evolution of the Earth's atmosphere, evolutionary pathways of marine life and cycles of major mineral deposits. Using laser-based analysis of sedimentary pyrite in deep marine rocks, this project aims to produce, for the first time, temporal variation curves for 25 trace elements in seawater over the ....Pyrite: a deep-time capsule of ocean chemistry and atmosphere oxidation. Surprisingly little is known about trace element trends in past oceans, even though these data are vital for interpreting the evolution of the Earth's atmosphere, evolutionary pathways of marine life and cycles of major mineral deposits. Using laser-based analysis of sedimentary pyrite in deep marine rocks, this project aims to produce, for the first time, temporal variation curves for 25 trace elements in seawater over the last 3.5 billion years. Preliminary research has validated the technique and demonstrated major changes in certain trace elements over geologically short periods. Outcomes will assist the minerals industry in the discovery of new deposits of zinc, copper, gold and iron ore in Australia.Read moreRead less
Integrating Global Multidimensional Datasets to Underpin Subduction Process Modelling During the Past 60 Million Years. Subduction zones are the sites for massive sulphide, orogenic vein gold and porphyry deposits. As Australia derived 47% of it merchandise exports from its mineral and energy resources in 2001, ore-deposits constitute an important component of the Australian economy. Understanding the environment of subduction initiation and development as well as the signal that it imparts on ....Integrating Global Multidimensional Datasets to Underpin Subduction Process Modelling During the Past 60 Million Years. Subduction zones are the sites for massive sulphide, orogenic vein gold and porphyry deposits. As Australia derived 47% of it merchandise exports from its mineral and energy resources in 2001, ore-deposits constitute an important component of the Australian economy. Understanding the environment of subduction initiation and development as well as the signal that it imparts on the magmatic (ore-forming) arc, will provide improved efficiency for targeting Australia's deep-earth ore-deposits.Read moreRead less
Partial melting in natural metal-silicate and silicate systems: rheological and geochemical implications for the Earth and other planets. Understanding how fluid and melts migrate through the Earth's crust is vital to predicting how important minerals, metals and oil can be concentrated. Understanding fluid-rock systems therefore contribute to an environmentally sustainable Australia (Research Priority 1). Furthering our knowledge of permeable networks through the use of dynamic experiments is a ....Partial melting in natural metal-silicate and silicate systems: rheological and geochemical implications for the Earth and other planets. Understanding how fluid and melts migrate through the Earth's crust is vital to predicting how important minerals, metals and oil can be concentrated. Understanding fluid-rock systems therefore contribute to an environmentally sustainable Australia (Research Priority 1). Furthering our knowledge of permeable networks through the use of dynamic experiments is an innovative way to study their development within naturally evolving crustal systems as they respond to changing physical and chemical conditions. Thus, this proposal is also directly concerned with the continuing aim of building a sustainable Australia through knowledge of deep Earth resources.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.