Distribution and origin of 4 billion-year-old zircons from Western Australia: Implications for the early history of the earth and moom. We aim to determine the distribution and origin of >4 billion year old (Ga) zircons in rocks from north-western Western Australia, using geological mapping, mineralogical and chemical techniques and SHRIMP zircon geochronology. The >4Ga zircons are the oldest known crustal material, and the only material which can give direct information on the earliest evoluti ....Distribution and origin of 4 billion-year-old zircons from Western Australia: Implications for the early history of the earth and moom. We aim to determine the distribution and origin of >4 billion year old (Ga) zircons in rocks from north-western Western Australia, using geological mapping, mineralogical and chemical techniques and SHRIMP zircon geochronology. The >4Ga zircons are the oldest known crustal material, and the only material which can give direct information on the earliest evolution of the Earth. In this research, we will collaborate with international research groups also intending to investigate the early history of the Earth using the >4Ga zircons. Outcomes will be new ideas on the origin of the zircons, the differentiation of the Earth, the formation of the Moon and the Earth's oceans, and the development of ancient life forms.Read moreRead less
An experimental study of trace element equilibria during metamorphism. The analytical methods and experimental data to be developed will enable an Australian team to become world leaders in determining pressures and temperatures of mineral growth that correspond to a range of depths and temperature gradients in the Earth tha t is wider than accessible previously. Obtaining this information from small zones within single grains will allow determination of rates of change, and give us a detailed p ....An experimental study of trace element equilibria during metamorphism. The analytical methods and experimental data to be developed will enable an Australian team to become world leaders in determining pressures and temperatures of mineral growth that correspond to a range of depths and temperature gradients in the Earth tha t is wider than accessible previously. Obtaining this information from small zones within single grains will allow determination of rates of change, and give us a detailed picture of how the host rock has evolved, even from very small samples. One application would be checking the origin of relatively common minerals for whether they could be associated with diamonds.Read moreRead less