Evolution of a two billion year subduction zone: Insights from the integration of microstructure and geochronology. The dynamic evolution of the earth is fundamentally linked to its thermal history. Since, the internal heat production of the earth has changed over time, plate tectonic processes may also have changed over earth history. The manner and timing of this change is highly controversial. We aim to address the nature of tectonic processes 2 billion years ago by studying one of the wor ....Evolution of a two billion year subduction zone: Insights from the integration of microstructure and geochronology. The dynamic evolution of the earth is fundamentally linked to its thermal history. Since, the internal heat production of the earth has changed over time, plate tectonic processes may also have changed over earth history. The manner and timing of this change is highly controversial. We aim to address the nature of tectonic processes 2 billion years ago by studying one of the world's oldest subduction zones (the Usagarian belt in Tanzania). The geometry, kinematics and deformation history of the subduction complex will be integrated with radiometric age dating to quantify the style and rates of ancient tectonic processes.Read moreRead less
Gondwana in East Asia? A biogeographic test using Permian marine invertebrate biota. Combining Permian fossil collections from key Australian, NE Chinese, East Russian and Japanese localities, coupled with a detailed quantitative biogeographical analysis, this project will provide fundamental data for evaluating current plate tectonic models regarding the palaeo-positions of some of the tectonic blocks in East Asia. In particular, this project will test, using biogeographical data, the validity ....Gondwana in East Asia? A biogeographic test using Permian marine invertebrate biota. Combining Permian fossil collections from key Australian, NE Chinese, East Russian and Japanese localities, coupled with a detailed quantitative biogeographical analysis, this project will provide fundamental data for evaluating current plate tectonic models regarding the palaeo-positions of some of the tectonic blocks in East Asia. In particular, this project will test, using biogeographical data, the validity of several recently proposed claims that continental East Asia contains some tectonic blocks of Gondwana origin. An improved understanding of the Permian palaeogeographical relationship between Gondwanaland and East Asia is critical for improving geological models for resources exploration and the understanding of earth history.Read moreRead less
The Genesis and Tectonic Setting of Iron Oxide Associated Mineralisation in Germany and South Australia. FeOx associated mineralisations are not restricted to Olympic Dam and Ernest Henry types but occur in various geological settings, e.g. the Mt Painter and Olary region, S A. Ocurrences in Central Europe (Erzgebirge, Harz/Calvörde) contain U and other metals, their structural setting is well recorded. Together with the Bergakademie Freiberg, Germany, and the University of Nancy, France, these ....The Genesis and Tectonic Setting of Iron Oxide Associated Mineralisation in Germany and South Australia. FeOx associated mineralisations are not restricted to Olympic Dam and Ernest Henry types but occur in various geological settings, e.g. the Mt Painter and Olary region, S A. Ocurrences in Central Europe (Erzgebirge, Harz/Calvörde) contain U and other metals, their structural setting is well recorded. Together with the Bergakademie Freiberg, Germany, and the University of Nancy, France, these mineralisations shall be investigated with modern geological and geochemical methods to develop a unifying model for the genesis of iron oxide associated U-metal-REE deposits. This will help identifying exploration targets and distinguish different types of mineralisation upon their genetic setting.Read moreRead less
How has continental lithosphere evolved? Processes of assembly, growth, transformation and destruction. Novel in-situ analytical and dating techniques will be used on samples from the Earth's mantle and deep crust to define the processes by which the continents and their roots (to depths of 250 km) have been formed, modified or destroyed at different times throughout Earth's 4.6 billion year evolution. The role of oceanic plateaus and mantle plumes in building protocontinents or modifying lithos ....How has continental lithosphere evolved? Processes of assembly, growth, transformation and destruction. Novel in-situ analytical and dating techniques will be used on samples from the Earth's mantle and deep crust to define the processes by which the continents and their roots (to depths of 250 km) have been formed, modified or destroyed at different times throughout Earth's 4.6 billion year evolution. The role of oceanic plateaus and mantle plumes in building protocontinents or modifying lithospheric volumes will be evaluated. The results will provide a more robust framework for interpreting the architecture of Earth's lithosphere and will have relevance to the formation and location of resources such as Ni, PGEs, Au and diamonds.Read moreRead less
Biogeography and evolution of Australia's fossil reptiles: A global perspective. Large marine reptiles such as plesiosaurs, and missing links such as legged snakes, are spectacular animals that have captured public attention. This collaboration will directly enhance public museum displays by collecting and preparing these spectacular fossils; many of the fossils found by the CIs are now centerpieces of museum displays (e.g. the SA museum). Also, it will also promote awareness and sustainable u ....Biogeography and evolution of Australia's fossil reptiles: A global perspective. Large marine reptiles such as plesiosaurs, and missing links such as legged snakes, are spectacular animals that have captured public attention. This collaboration will directly enhance public museum displays by collecting and preparing these spectacular fossils; many of the fossils found by the CIs are now centerpieces of museum displays (e.g. the SA museum). Also, it will also promote awareness and sustainable use of the environment: it will facilitate CI Kear in running earthwatch-style ecotourism field trips which promote sustainable use of finite fossil resources by making them commercially valuable to local communities as a source of tourism revenue.Read moreRead less
Accessory Mineral Microstructure and Implications for Geochronology. U-Pb geochronology of accessory minerals is widely used to constrain the timing of igneous, metamorphic and sedimentary processes. However, our current knowledge of isotope mobility in these important minerals cannot readily explain some common features of U-Pb dating. Using new developments in quantitative microstructural analysis integrated with high spatial resolution geochronology we will constrain the relationship between ....Accessory Mineral Microstructure and Implications for Geochronology. U-Pb geochronology of accessory minerals is widely used to constrain the timing of igneous, metamorphic and sedimentary processes. However, our current knowledge of isotope mobility in these important minerals cannot readily explain some common features of U-Pb dating. Using new developments in quantitative microstructural analysis integrated with high spatial resolution geochronology we will constrain the relationship between accessory minerals deformation and its effect on radiometric ages. Our results will lead to a better understanding of geochemical modification of accessory minerals and may lead to the development of new applications of geochronology and improve the dating of rock deformation.Read moreRead less