School of Earth and Environment
High Temperature Geochemistry
The High Temperature Geochemistry Group studies the role of water and other volatiles in the Earth’s crust and mantle, where they have a major impact on both physical and chemical processes.
Current projects include:
- (i) Water-rock interactions at both mid-ocean ridges and subduction zones: how does water circulation modify rock compositions and affect how they deform?
- (ii) Groundwater circulation around volcanoes: can studies of ancient volcanoes maximise geothermal energy production at modern ones?
- (iii) Geochemistry of ore fluids: are unusual metal concentrations needed to form ore bodies and why do they precipitate?
- (iv) Mineral reactions in the mid-to lower crust: how does water drive metamorphic reactions and how do they affect the strength of the crust?
The School has excellent facilities to support this work: Triton Thermal Ionisation Mass Spectrometer, Agilent ICP-MS with Geolas Excimer laser ablation system as well as a SEM and Microprobe.

High resolution (ToF-SIMS elemental map of a unique veined serpentinite rock from ODP Leg 195 in the Mariana subduction zone.

RV JOIDES "Resolution" in the Azores.
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