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.
Understanding planetary-scale reorganisations in plate tectonics. This project aims to investigate the dynamics of Earth’s tectonics and its plate motions, with the aim of understanding the mechanisms that force single plates or whole-Earth motions’ changes. The Earth’s tectonics follow regular cycles, in every ~500 million years, of continental aggregation and dispersal, which are intervened by periodic destabilisation and rapid reorganisations. What causes the reorganisations and reversal of t ....Understanding planetary-scale reorganisations in plate tectonics. This project aims to investigate the dynamics of Earth’s tectonics and its plate motions, with the aim of understanding the mechanisms that force single plates or whole-Earth motions’ changes. The Earth’s tectonics follow regular cycles, in every ~500 million years, of continental aggregation and dispersal, which are intervened by periodic destabilisation and rapid reorganisations. What causes the reorganisations and reversal of the tectonics remain standing questions in planetary dynamics. The expected outcomes of the project will provide an understanding of the recent supercontinent formation and its fragmentation into the present-day continents.Read moreRead less
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
Discovery Early Career Researcher Award - Grant ID: DE130100604
Funder
Australian Research Council
Funding Amount
$375,000.00
Summary
The dynamics of continent deformations. Modeling the coupling of subducting oceanic plates and deforming continents provides a fundamentally new view of the dynamics of our planet. It will improve an understanding of the formation of basins in continent interiors and their evolution over geological times.
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.
Discovery Early Career Researcher Award - Grant ID: DE120102245
Funder
Australian Research Council
Funding Amount
$375,000.00
Summary
Comparison of early mesozoic sedimentary provenances of both sides of the YarlungTsangpo suture zone and the evolution of the neotethys. This project aims to develop a new, more geologically-consistent evolution of the Neotethys and test the affinity of southern Lhasa terrane with Australian terranes. The work will provide new constraints on the early evolution of the Himalayan-Tibetan continental collision.
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.
Australian Laureate Fellowships - Grant ID: FL160100168
Funder
Australian Research Council
Funding Amount
$2,851,557.00
Summary
The pulse of the earth. The pulse of the earth. This project aims to establish the origin and evolution of the continental crust and its role in the long term development of the Earth system. The continental crust hosts the resources on which we depend and its evolution controls the environment in which we live. The crust’s record (including resources) is episodic in space and time, but the origin of this periodicity is unresolved. Building on recent advances on crustal development, the fellowsh ....The pulse of the earth. The pulse of the earth. This project aims to establish the origin and evolution of the continental crust and its role in the long term development of the Earth system. The continental crust hosts the resources on which we depend and its evolution controls the environment in which we live. The crust’s record (including resources) is episodic in space and time, but the origin of this periodicity is unresolved. Building on recent advances on crustal development, the fellowship would work to resolve the origin of the episodic age pattern, which affects the distribution of mineral systems and their prospectivity.Read moreRead less
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