Revealing the deep Earth in deep time

该项目旨在确定地球历史头25%结束时地球内部化学和动力变化的性质。这将为现代地表特征的相关建立提供新的理解，例如广阔的大陆和含氧大气，并调查与西澳大利亚州矿产资源的因果关系。 预期的结果将是对我们星球的化学和热历史的重要新认识。

This project aims to determine the nature of the chemical and dynamical transformation of the Earth’s interior at the end of the first 25 per cent of its history. This will provide a new understanding of the related establishment of modern surface features such as extensive continents and an oxygenated atmosphere, as well as investigate causal relationships with west Australia’s mineral resources. The expected outcome will be a significant new understanding of the chemical and thermal history of our planet.