Unravelling the nature of secular global climatic change on the Precambrian Earth. Ancient sedimentary rocks record evidence of major climate change and variations in the composition of the atmosphere. By applying novel isotopic and geochemical techniques, this project aims to document when and how the Earths atmosphere and climate changed prior to the evolution of complex lifeforms. Curiously, such dramatic climate changes have controlled both the rate of evoutionary process and the formation o ....Unravelling the nature of secular global climatic change on the Precambrian Earth. Ancient sedimentary rocks record evidence of major climate change and variations in the composition of the atmosphere. By applying novel isotopic and geochemical techniques, this project aims to document when and how the Earths atmosphere and climate changed prior to the evolution of complex lifeforms. Curiously, such dramatic climate changes have controlled both the rate of evoutionary process and the formation of world class mineral deposits.Read moreRead less
The early evolution of the Earth system from multiple sulfur isotope records of sediments and seafloor mineral systems. This project addresses the early evolution of the Earth system that is one of the most important questions in Earth Sciences. It will use Australia's unique rock record and analytical techniques developed in Australia in collaboration with leading international researchers. The National Research Priority area 'An environmentally sustainable Australia: developing deep Earth reso ....The early evolution of the Earth system from multiple sulfur isotope records of sediments and seafloor mineral systems. This project addresses the early evolution of the Earth system that is one of the most important questions in Earth Sciences. It will use Australia's unique rock record and analytical techniques developed in Australia in collaboration with leading international researchers. The National Research Priority area 'An environmentally sustainable Australia: developing deep Earth resources' will benefit through the development of better exploration models for Archaean submarine metal deposits. Students will obtain a high level understanding of the early Earth system, ore deposits, stable isotope and transition metal geochemistry, which are directly applicable in both pure and applied research and mineral exploration.Read moreRead less
Linkage Infrastructure, Equipment And Facilities - Grant ID: LE0560786
Funder
Australian Research Council
Funding Amount
$495,000.00
Summary
A ThermoFinnigan Triton high-sensitivity thermal ionisation mass spectrometer for constraining geoscience rates and environmental processes via Ra and Os analysis. The short-lived isotope 226Ra provides a powerful new tool for constraining the nature of melting and magma/fluid transport processes within the Earth. Conversely, Os isotopes can track ancient recycled components, core-mantle boundary interaction and date organic-rich sediments. The installation of a high-sensitivity thermal ionisati ....A ThermoFinnigan Triton high-sensitivity thermal ionisation mass spectrometer for constraining geoscience rates and environmental processes via Ra and Os analysis. The short-lived isotope 226Ra provides a powerful new tool for constraining the nature of melting and magma/fluid transport processes within the Earth. Conversely, Os isotopes can track ancient recycled components, core-mantle boundary interaction and date organic-rich sediments. The installation of a high-sensitivity thermal ionisation mass spectrometer at Macquarie University will enable research in these exciting endeavours and enhance a world-class analytical facility with widespread and lasting utility. Planned research will constrain deep earth processes, magma/water transport processes, magma-mantle/chromatography, volcanic hazards, ore deposit formation, controversial climatic models, soil erosion and early planet differentiation.Read moreRead less
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
Tectonic Reconstruction of the Evolution of the Alpine-Himalayan Orogenic Chain. This project will construct a computationally explicit model of movements in the solid Earth for the past 150 million years, to study the Earth as a complex system during the collision that produced the Alpine-Himalayan mountain belt. This is the youngest collisional mountain belt on Earth, and at times it stretched from Spain to New Zealand. Earth Scientists want to understand the processes that took place to mak ....Tectonic Reconstruction of the Evolution of the Alpine-Himalayan Orogenic Chain. This project will construct a computationally explicit model of movements in the solid Earth for the past 150 million years, to study the Earth as a complex system during the collision that produced the Alpine-Himalayan mountain belt. This is the youngest collisional mountain belt on Earth, and at times it stretched from Spain to New Zealand. Earth Scientists want to understand the processes that took place to make it, in particular the role of ribbon continents. As a result of this work ordinary Australians will be able to better perceive their interactions with their nearest neighbours.Read moreRead less
Weathering History and Cenozoic Landscape Evolution in Northern Queensland and New Caledonia. Rates of rock weathering impose a major control on the CO2 global budget. Increased weathering rates consume atmospheric CO2, possibly resulting in cooler climates. We intend to determine rock weathering rates on similar lithologies currently placed on equatorial positions, Northeastern Australia and New Caledonia, but possibly differing in climatic history. Geochronology of continental weathering prof ....Weathering History and Cenozoic Landscape Evolution in Northern Queensland and New Caledonia. Rates of rock weathering impose a major control on the CO2 global budget. Increased weathering rates consume atmospheric CO2, possibly resulting in cooler climates. We intend to determine rock weathering rates on similar lithologies currently placed on equatorial positions, Northeastern Australia and New Caledonia, but possibly differing in climatic history. Geochronology of continental weathering profiles in the areas will permit correlating known paleoclimatic cycles, derived from the isotopic composition of ocean floor sediments, with the variation in continental weathering rates. This comparison will test current models proposing that cooling of Cenozoic climates results from increase rates of rock weathering.Read moreRead less
Oxygenating the Earth: using innovative techniques to resolve the timing of the origin of oxygen-producing photosynthesis in cyanobacteria. The early Earth was a hostile place with little oxygen in the atmosphere. Then cyanobacteria ('blue-green algae') invented oxygen-releasing photosynthesis. That profound event affected many fundamental processes, from the course of evolution to the formation of ore deposits. However, estimates of when these bacteria originated are disputed with uncertainties ....Oxygenating the Earth: using innovative techniques to resolve the timing of the origin of oxygen-producing photosynthesis in cyanobacteria. The early Earth was a hostile place with little oxygen in the atmosphere. Then cyanobacteria ('blue-green algae') invented oxygen-releasing photosynthesis. That profound event affected many fundamental processes, from the course of evolution to the formation of ore deposits. However, estimates of when these bacteria originated are disputed with uncertainties of hundreds of millions of years. We will resolve those uncertainties. We have developed new analytical techniques that we will apply to well-preserved 2.7-2.8 billion-year-old rocks in Western Australia. We will couple that approach to the use of the latest genetic techniques to reveal the origins of living cyanobacteria.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
Developing indicator minerals to geochemically fingerprint mineralized Fe oxide Cu-Au systems: a pilot study around the Ernest Henry Cu-Au mine. Fe oxide Cu-Au deposits represent some of the largest accumulations of economically extractable metal in the earth's crust. However, exploration has been largely ineffective over the last decade, and new methods for their delineation are required to deliver a step-change in the efficiency of exploration programs. The development of a mineral indicator s ....Developing indicator minerals to geochemically fingerprint mineralized Fe oxide Cu-Au systems: a pilot study around the Ernest Henry Cu-Au mine. Fe oxide Cu-Au deposits represent some of the largest accumulations of economically extractable metal in the earth's crust. However, exploration has been largely ineffective over the last decade, and new methods for their delineation are required to deliver a step-change in the efficiency of exploration programs. The development of a mineral indicator scheme to fingerprint potential ?ore-forming? systems using state-of-the-art laser ablation ICP-MS analysis may engender new methods and strategies that lead to exploration success. A baseline study around a known deposit provides the best means to characterize indicators- the Ernest Henry Cu-Au deposit provides the ideal candidate.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