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Department of Earth Sciences, University College London, Gower Street, London WC1E6BT, UK
Department of Earth Sciences, University College London, Gower Street, London WC1E 6BT, UK; Department of Chemistry, University College London, 20 Gordon Street, London WC1H 0AJ, UK
Department of Earth Sciences, University College London, Gower Street, London WC1E 6BT, UK; Mineral Physics Institute, Department of Earth and Space Sciences, Stony Brook University, Stony Brook, NY, USA
Department of Earth Sciences, University College London, Gower Street, London, WC1E 6BT, UK; Mineral Physics Institute, Dept. Geosci., SUNY Stony Brook, Stony Brook, NY 11790, USA
An Experimental Investigation of the Pressure Effect on Stable Isotope Fractionation at High Temperature; Implications for Mantle Processes and Core Formation in Celestial Bodies from 1 GPa and Up to 25 Gpa
Deformation of olivine at 5 GPa and 350 900 °C
On the increase in thermal diffusivity caused by the perovskite to post-perovskite phase transition and its implications for mantle dynamics
Relative strength of the pyrope-majorite solid solution and the flow-law of majorite containing garnets
Towards better analogues for MgSiO3 post-perovskite: NaCoF3 and NaNiF3, two new recoverable fluoride post-perovskites
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