Experimental and empirical insight into melting of the early Earth's mantle. The early Earth's mantle produced melt at much higher temperature than today, creating rocks with unique chemistries and mineralogies. But pressing knowledge gaps about hot mantle melting remain. The aim of this project is to generate new experimental and empirical knowledge to help closing these gaps by:
(i) conducting high pressure experiments to refine phase-composition relationships and element partitioning;
(ii) qu ....Experimental and empirical insight into melting of the early Earth's mantle. The early Earth's mantle produced melt at much higher temperature than today, creating rocks with unique chemistries and mineralogies. But pressing knowledge gaps about hot mantle melting remain. The aim of this project is to generate new experimental and empirical knowledge to help closing these gaps by:
(i) conducting high pressure experiments to refine phase-composition relationships and element partitioning;
(ii) quantifying mineral fabrics in cratonic peridotites to understand the movement of early continents; and
(iii) constructing the first petrological deep time model for greenstone belt volcanic rocks.
The expected outcomes are better models for the early Earth's melting and tectonic regimes and insight into the emergence of land.Read moreRead less
The link between cratonic roots, redox state, and mantle geodynamics. This project aims to understand the role of Earth's redox state on the geodynamic evolution of continental cratonic roots. Cratonic roots form strong, buoyant rafts upon which Australia's oldest crust and mineral deposits survived. Cratons preserve a record of planetary-scale chemical shifts, including the rise of surface oxygen, but it is unclear how these redox shifts themselves affected lithospheric processes. This project ....The link between cratonic roots, redox state, and mantle geodynamics. This project aims to understand the role of Earth's redox state on the geodynamic evolution of continental cratonic roots. Cratonic roots form strong, buoyant rafts upon which Australia's oldest crust and mineral deposits survived. Cratons preserve a record of planetary-scale chemical shifts, including the rise of surface oxygen, but it is unclear how these redox shifts themselves affected lithospheric processes. This project integrates new developments in geochemistry, geophysics, and geodynamics, to map the geochemical state and structure of cratonic roots, aiding mineral exploration, and also shedding light on the processes that modify, mineralise, and sometimes destroy cratonic roots.Read moreRead less
Revealing the deep Earth in deep time. This project aims to determine the nature of the chemical and dynamical transformation of the Earth’s interior at the end of the first 25 per cent of its history. This will provide a new understanding of the related establishment of modern surface features such as extensive continents and an oxygenated atmosphere, as well as investigate causal relationships with west Australia’s mineral resources. The expected outcome will be a significant new understandin ....Revealing the deep Earth in deep time. This project aims to determine the nature of the chemical and dynamical transformation of the Earth’s interior at the end of the first 25 per cent of its history. This will provide a new understanding of the related establishment of modern surface features such as extensive continents and an oxygenated atmosphere, as well as investigate causal relationships with west Australia’s mineral resources. The expected outcome will be a significant new understanding of the chemical and thermal history of our planet.Read moreRead less
Earth's Dynamic Topography Through Space and Time. A key component of Earth’s topography remains enigmatic. This so-called dynamic topography is transient, varying in response to convection within Earth’s mantle. This project aims to use a data-driven computational approach to: (i) reconstruct the evolution of dynamic topography over the recent geological history of our planet (Cenozoic Era, 0-66 million years ago); and (ii) uncover the mechanisms controlling its spatial and temporal evolution. ....Earth's Dynamic Topography Through Space and Time. A key component of Earth’s topography remains enigmatic. This so-called dynamic topography is transient, varying in response to convection within Earth’s mantle. This project aims to use a data-driven computational approach to: (i) reconstruct the evolution of dynamic topography over the recent geological history of our planet (Cenozoic Era, 0-66 million years ago); and (ii) uncover the mechanisms controlling its spatial and temporal evolution. This transformational new understanding will connect the evolution of our planet's surface environments to its deep interior, revealing the impact of dynamic topography on sea level change, flooding, river networks, groundwater systems, habitat development and the distribution of economic resources. Read moreRead less
Eruption and disruption: how Earth’s deep interior and surface communicate. Massive volcanic eruptions are a fundamental part of the Earth System, responsible for globally disruptive events, from airspace disturbance, to extinction of the dinosaurs. This project will reveal relationships between hot, deep sources of volcanic material, and the tectonic processes at the Earth's surface. Expected outcomes of this project include assembling an unprecedented set of new observations from underwater vo ....Eruption and disruption: how Earth’s deep interior and surface communicate. Massive volcanic eruptions are a fundamental part of the Earth System, responsible for globally disruptive events, from airspace disturbance, to extinction of the dinosaurs. This project will reveal relationships between hot, deep sources of volcanic material, and the tectonic processes at the Earth's surface. Expected outcomes of this project include assembling an unprecedented set of new observations from underwater volcanoes offshore Eastern Australia, and the development of innovative geodynamic models of how the deep Earth interacts with the surface to form these volcanoes. This will provide significant benefits by advancing our understanding of the deep Earth, and its impact on Earth’s surface, natural hazards, and mineral systems.Read moreRead less
Earthquake biases in measurements of Antarctica's sea-level contribution. This project aims to accurately determine Antarctica’s contribution to present-day sea-level. Large technique-specific systematic errors make this uncertain and controversial with the sign of change not agreed. Three of four measurement techniques rely on knowing the solid earth's changing shape or gravity field. Studies have not considered post-seismic deformation, but GPS data show that Antarctica has deformed since the ....Earthquake biases in measurements of Antarctica's sea-level contribution. This project aims to accurately determine Antarctica’s contribution to present-day sea-level. Large technique-specific systematic errors make this uncertain and controversial with the sign of change not agreed. Three of four measurement techniques rely on knowing the solid earth's changing shape or gravity field. Studies have not considered post-seismic deformation, but GPS data show that Antarctica has deformed since the 1998 Magnitude-8.2 Antarctic Plate Earthquake. This project will develop a model of these earthquakes constrained by geodetic data and use the model to estimate Antarctica's contribution to sea-level change. This should enable more confident local, national and international planning. This will benefit society through reducing the sea-level projection uncertainty.Read moreRead less