Thermoelastic properties of subducted crustal materials

The chemistry, mineralogy and temperature of Earth’s interior are the most fundamental properties of our planet. It is these properties that control Earth’s evolution, not only of its interior but also of its atmosphere, climate and surface environment over geological time. However, studying the deep Earth is not a straightforward task as direct sampling is limited to ~ 10km depth. We instead rely on petrology and geophysics – predominantly the interpretation of seismology – to understand anything except the near surface. Fortunately, seismic observations are high quality and abundant. The problem is that the experimental data needed for reliable interpretations remains sparse. In particular, the available thermoelastic data for minerals thought to be abundant in the oceanic and continental crust (e.g. pyroxene, amphibole, serpentine, chlorite, feldspar) at mantle conditions are very poorly studied. 

This PhD will utilise the NHM’s mineral collections, high pressure labs at UCL and diffraction capabilities at the NHM/UCL to measure the thermoelastic properties of Earth minerals at high pressure and high temperature conditions. Lab experiments will be supplemented by application for instrument time at international synchrotron and/or neutron sources as appropriate. The data collected will be used to interpret geophysical observations of Earth’s interior.