CORDIS Project
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This research focuses on measuring the physical properties of the Earth's inner mantle to improve our understanding of geological processes. It utilizes advanced techniques to obtain accurate data on mineral sound velocities and densities at high pressures and temperatures.
Knowledge of the physical and chemical state of the Earth s inner silicate mantle is central to our understanding of plate tectonics, mantle convection, magma generation and the composition of the Earth as a whole.
The key to this knowledge is the ability to interpret studies of seismic wave velocities through the deep Earth using laboratory measurements of mineral sound velocities at high pressures and temperatures.
Scientists have for many years measured these properties as a function of press…
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