Geodynamics and continental extension in the East African Rift System: origin and evolution of the Turkana Depression in northern Kenya. The Lake Turkana region in northern Kenya, famous for its fossil evidence of human origins, occupies a critical position within the Great Rift Valley of East Africa. This project seeks to explain how this complex region evolved and also the dynamic earth processes responsible for its formation between two great uplifted domes in Ethiopia and Kenya.
The global consequences of subduction zone congestion. This project will use a combination of 3D geodynamic modelling, plate kinematic reconstruction and geological and geophysical synthesis to determine how congested subduction zones influence plate kinematics, subduction dynamics and tectonic evolution at orogen and global scales. The project aims to deliver a transformation change in understanding the links between congested subduction, mantle flow, trench migration, crustal growth, transitio ....The global consequences of subduction zone congestion. This project will use a combination of 3D geodynamic modelling, plate kinematic reconstruction and geological and geophysical synthesis to determine how congested subduction zones influence plate kinematics, subduction dynamics and tectonic evolution at orogen and global scales. The project aims to deliver a transformation change in understanding the links between congested subduction, mantle flow, trench migration, crustal growth, transitions between stable convergent margin configurations and deformation in the overriding plates of subduction zones. Determining these relationships is significant because it will provide dynamic context to interpret the geological record of ancient convergent margins, which host a large percentage of Earth's metal resources.Read moreRead less
Magmatic response to slab deformation and implications to ore formation. The uneven distribution of ore deposits in magmatic arcs is poorly understood. This project aims to provide new strategies for more effective mineral targeting by testing the hypothesis that anomalous magmatism enriched in metals reflects particular styles of deformation, such as tears in subducting slabs. We will use geophysical modelling to constrain slab structure along the northern boundary of the Australian plate, and ....Magmatic response to slab deformation and implications to ore formation. The uneven distribution of ore deposits in magmatic arcs is poorly understood. This project aims to provide new strategies for more effective mineral targeting by testing the hypothesis that anomalous magmatism enriched in metals reflects particular styles of deformation, such as tears in subducting slabs. We will use geophysical modelling to constrain slab structure along the northern boundary of the Australian plate, and geochemical data to establish spatio-temporal links with anomalous magmatism and ore deposits. By identifying the geochemical fingerprint of tear-related magmatism, outcomes are expected to benefit geoscience research and mineral exploration by providing context to similar rock associations in mineral-rich provinces.Read moreRead less
Indo-Australian Plate Active Tectonics Program. The Indo-Australian Plate Active Tectonics Program investigates fundamental questions in geodynamics using the unique record of landscape evolution in Australia. In this project the origin of iconic landscapes such as the Lake Eyre Basin and the Flinders Ranges will be addressed to explore the nature of the couplings between surface deformation and flow in the upper mantle, and between surface processes and tectonic activity.
Three dimensional geospatial model of the Australian continent from geologically constrained inverse modelling of the Earth's gravity and magnetic fields. This project enhances Australia's reputation in integration of geology and geophysics and will create a three dimensional model of the Australian crust that will image and define the geometry of the fundamental building blocks of the continent. The outcomes will create new concepts for resource exploration and hazard recognition.
Cyclicity in magmatic arc systems. This project aims to determine how active volcanic continental margins, such as the Ring of Fire, evolves and control the origin of new continental crust. This project expects to generate new knowledge regarding how continents form in such margins using new findings that suggest they undergo cyclical heating and magmatism. The intended outcome is a finely resolved thermal-magmatic temporal history of an ideal example of such a margin. This should provide signif ....Cyclicity in magmatic arc systems. This project aims to determine how active volcanic continental margins, such as the Ring of Fire, evolves and control the origin of new continental crust. This project expects to generate new knowledge regarding how continents form in such margins using new findings that suggest they undergo cyclical heating and magmatism. The intended outcome is a finely resolved thermal-magmatic temporal history of an ideal example of such a margin. This should provide significant benefits, such as an understanding of how new continental crust forms, and increased predictability of when in the evolution of continental margins significant copper and gold deposits form.Read moreRead less
The impact of India-Asia tectonics on climate. This interdisciplinary project aims to determine the controls of tectonics on global climate in the last 50 million years. A combination of tectonics, paleogeography, climate modelling and high-performance computing will be applied to test systematically outstanding issues in the reconstruction of the Indo-Asia region and their landmass/seaways configurations and topography, which have bedevilled previous models of paleoclimate evolution. The propos ....The impact of India-Asia tectonics on climate. This interdisciplinary project aims to determine the controls of tectonics on global climate in the last 50 million years. A combination of tectonics, paleogeography, climate modelling and high-performance computing will be applied to test systematically outstanding issues in the reconstruction of the Indo-Asia region and their landmass/seaways configurations and topography, which have bedevilled previous models of paleoclimate evolution. The proposal expects to generate novel knowledge in the area at the boundary between tectonics, paleoclimate modelling and present-day climate. This provides significant benefits to the interpretation of tectonics–climate coupling as current drivers of climate evolution.Read moreRead less
Active tectonics of East Timor: geomorphic responses to an evolving slab rupture. Through analysis of the landscape evolution of East Timor, this project will establish new insights into basic dynamic processes responsible for formation of mountain systems. By quantifying slip rates on active faults and erosion rates across its landscape, it will provide new constraints on natural hazards for East Timor, and the broader region.
Intraplate volcanism near lateral slab edges: result of deep mantle plumes or slab rollback-induced mantle flow? This project investigates how the Earth's interior (the mantle) flows near edges of tectonic plates as these plates sink into the mantle. This is important because these flows have been crucial in shaping the Southwest Pacific region bordering Australia and might be responsible for the formation of some of the largest volcanoes on Earth.
Add mountains and shake: plate boundary fault and earthquake patterns. This project aims to determine the fundamental physical processes that link topography, seismic shaking and volcanism to the evolution of seismogenic fault networks in obliquely convergent (transpressional) plate boundary settings. We will combine detailed field and remote sensing-based structural analyses in transpressional mountain belts with advanced laboratory analogue and numerical experiments to evaluate: 1) how bursts ....Add mountains and shake: plate boundary fault and earthquake patterns. This project aims to determine the fundamental physical processes that link topography, seismic shaking and volcanism to the evolution of seismogenic fault networks in obliquely convergent (transpressional) plate boundary settings. We will combine detailed field and remote sensing-based structural analyses in transpressional mountain belts with advanced laboratory analogue and numerical experiments to evaluate: 1) how bursts of strong seismic shaking perturb fault zone evolution through time; 2) the contribution of topography and gravitation loading to fault interactions and earthquake generation; and 3) feedbacks between fault network development, the spatial distribution of volcanic centres, seismic shaking and ore deposits.Read moreRead less