Deep Crustal Section Through a Late Archaean Orogen (Greenland): Archaean Crustal Sutures, Abyssal Peridotites and Gold. Did plate tectonics operate in Earth's early times - the Archaean (before 2500 million years ago)? This is important for understanding Australia's rich Archaean gold mineralisation. Using plate tectonics, young mountains like the European Alps formed when once distant continents collided. The project will investigate the origins of a deeply-eroded, superbly-exposed Archaean Gr ....Deep Crustal Section Through a Late Archaean Orogen (Greenland): Archaean Crustal Sutures, Abyssal Peridotites and Gold. Did plate tectonics operate in Earth's early times - the Archaean (before 2500 million years ago)? This is important for understanding Australia's rich Archaean gold mineralisation. Using plate tectonics, young mountains like the European Alps formed when once distant continents collided. The project will investigate the origins of a deeply-eroded, superbly-exposed Archaean Greenland mountain belt and its gold mineralisation. This is to establish whether it represents a deep section through an Archaean continent-continent collision formed via ancient plate tectonics and also to provide insight into Australia's important Archaean gold deposits and to produce models to help search for more gold.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
From Synchrotron Characterisation of Single Fluid Inclusions to Archaean Geodynamics: An Integrated Study of Fluid-Rock Interaction in the Primitive Crust. In the primitive Earth, a wide range of phenomena including the initiation of biological activity and the formation of ore deposits were related to the mobilisation of mineralised fluids through the crust. In the Archaean craton of the Pilbara (WA), we have identified, within its tectonic framework, a crustal-scale plumbing system that channe ....From Synchrotron Characterisation of Single Fluid Inclusions to Archaean Geodynamics: An Integrated Study of Fluid-Rock Interaction in the Primitive Crust. In the primitive Earth, a wide range of phenomena including the initiation of biological activity and the formation of ore deposits were related to the mobilisation of mineralised fluids through the crust. In the Archaean craton of the Pilbara (WA), we have identified, within its tectonic framework, a crustal-scale plumbing system that channelled large volumes of mineralised hydrothermal solutions. Our objective is to understand the development of this plumbing system in relation to Archaean crustal geodynamics using a combination of structural geology, metamorphic petrology, geochronology, geochemistry, and the analysis of single-fluid inclusion using synchrotron and other X-ray sources.Read moreRead less