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.
Resolving the influence of intraplate orogenesis on continental margin tectonics. Novel, multi-dating of continental sedimentary rocks will be undertaken to examine the effects of a high sediment flux from an enigmatic, major mountain-building event on a distant continental margin. This will expand our understanding of the range of tectonic influences between continental interiors and margins and onshore resource potential.
Supercells and the supercontinent cycle. This is a new approach to understanding how the Earth works, at a global-scale and billion-year perspective. In particular it seeks to understand why continents come together as supercontinents, then drift away again. The work has implications for copper-gold exploration on the Australian continent because it has relevant predictive capacity.
Building Central Asia: Linking the Growth of Asia to its Exhumation. The consumption of the Tethys Ocean and the associated collision of Gondwana-derived terranes with Eurasia resulted in the uplift of the highest mountain belt on Earth: the Himalayas. However, stresses from this collision zone propagated far into the Eurasian interior by reactivating faults and creating mountain belts along these fault zones. This project aims to map and model how and when fault (re)activation occurred by integ ....Building Central Asia: Linking the Growth of Asia to its Exhumation. The consumption of the Tethys Ocean and the associated collision of Gondwana-derived terranes with Eurasia resulted in the uplift of the highest mountain belt on Earth: the Himalayas. However, stresses from this collision zone propagated far into the Eurasian interior by reactivating faults and creating mountain belts along these fault zones. This project aims to map and model how and when fault (re)activation occurred by integrating multi-method thermochronological and structural data on major Meso-Cenozoic Central Asian fault systems. The resulting time-integrated tectonic model will aid in the understanding of the India-Eurasia collision, the building of the mountainous Central Asian landscape and its influence on the Asian climate.Read moreRead less
Multiple vertical tectonic movements in a continental interior: consequences of flat-subduction and foundering of an oceanic plateau? This project will investigate how the subduction of particularly thick oceanic crust impacts on the landscape, climate, structure and composition of the adjacent continent. It will help in understanding the history and distribution of mineral and hydrocarbon resources, of similar provinces in Australia.
A unified model for the closure dynamics of ancient Tethys constrained by geodesy, structural geology, argon geochronology and tectonic reconstruction. The project will elucidate complex planetary dynamics involved in the interaction of the oceanic plates with the continental crust. Such aspects underpin the ability of geoscientists to effectively simulate and model, impacting on issues ranging from forecasting earthquakes to how to conduct greenfields exploration for energy and mineral resource ....A unified model for the closure dynamics of ancient Tethys constrained by geodesy, structural geology, argon geochronology and tectonic reconstruction. The project will elucidate complex planetary dynamics involved in the interaction of the oceanic plates with the continental crust. Such aspects underpin the ability of geoscientists to effectively simulate and model, impacting on issues ranging from forecasting earthquakes to how to conduct greenfields exploration for energy and mineral resources.Read moreRead less
Jurassic arc? Reconstructing the lost world of Eastern Australia. This project aims to resolve a long-standing enigma about the geological formation of the Great Artesian Basin – Australia’s most important onshore reservoir for groundwater and hydrocarbon resources. Specifically, the project will integrate sedimentological and geochemical studies to investigate the geodynamic configuration of Eastern Australia during the Jurassic Period of basin formation. The intended outcomes are an improved u ....Jurassic arc? Reconstructing the lost world of Eastern Australia. This project aims to resolve a long-standing enigma about the geological formation of the Great Artesian Basin – Australia’s most important onshore reservoir for groundwater and hydrocarbon resources. Specifically, the project will integrate sedimentological and geochemical studies to investigate the geodynamic configuration of Eastern Australia during the Jurassic Period of basin formation. The intended outcomes are an improved understanding of the evolution of the Australian continent and better knowledge of the formation of intercontinental sedimentary basins, which includes better assessment of their potential to contain hydrocarbon resources.Read moreRead less
Garnet speed dating: Innovation for fast tectonic problem solving. This project aims to develop and apply a novel way to rapidly date the mineral garnet within rocks using the analytical technique of laser ablation mass spectrometry to calculate Lutetium-Hafnium ages. Garnet is the most important mineral we have to determine the depths of burial and the temperatures rocks experienced during the tectonic processes that shaped the continents. Our novel in situ laser ablation method will allow ga ....Garnet speed dating: Innovation for fast tectonic problem solving. This project aims to develop and apply a novel way to rapidly date the mineral garnet within rocks using the analytical technique of laser ablation mass spectrometry to calculate Lutetium-Hafnium ages. Garnet is the most important mineral we have to determine the depths of burial and the temperatures rocks experienced during the tectonic processes that shaped the continents. Our novel in situ laser ablation method will allow garnet to be rapidly and easily dated, permitting routine collection of large age datasets for tectonic problem solving. It will also offer a rapid means to determine ages of garnet-bearing rocks across prospective mineral exploration regions, providing explorers with key exploration data.Read moreRead less
What goes on inside subduction zones? This project aims to decipher how rocks behave inside subduction zones. Subduction is a central tenant of plate tectonic theory and the project will test the hypothesis rocks can become trapped within giant long-lived eddies that circulate material within subduction zones. This international collaborative project will generate new knowledge regarding the time scales rocks can remain trapped inside subduction zones using pressure–temperature–age constraints f ....What goes on inside subduction zones? This project aims to decipher how rocks behave inside subduction zones. Subduction is a central tenant of plate tectonic theory and the project will test the hypothesis rocks can become trapped within giant long-lived eddies that circulate material within subduction zones. This international collaborative project will generate new knowledge regarding the time scales rocks can remain trapped inside subduction zones using pressure–temperature–age constraints from subducted rocks. We will use this information as a framework for numerical simulations of subduction zone behaviour. The project will provide significant benefits in training a new generation of Earth scientists, and in broadening public awareness of fundamental Earth science.Read moreRead less
A detrital apatite archive to track crustal growth. This project will establish apatite as a new tool to study the evolution of the continental crust. The crust shaped the composition of the atmosphere and the oceans with consequences for the evolution of life through the availability of oxygen and nutrients. However, when and how the continental crust was generated remains a core question. Current models for continental crust development rely on the mineral zircon. However, zircons only record ....A detrital apatite archive to track crustal growth. This project will establish apatite as a new tool to study the evolution of the continental crust. The crust shaped the composition of the atmosphere and the oceans with consequences for the evolution of life through the availability of oxygen and nutrients. However, when and how the continental crust was generated remains a core question. Current models for continental crust development rely on the mineral zircon. However, zircons only record the history of evolved rocks. To address this bias we will use the mineral apatite which forms in less evolved rocks. We will develop a detrital apatite database of Pb-Nd (model) ages and integrate this with the zircon record to provide a more holistic description for how our planet developed.Read moreRead less