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Petrology
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Petrology
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Facilities

The Petrology Group hosts world-class facilities for performing and analysing experiments at conditions ranging from the Earth’s surface to its core, supported by a well-equipped and well-staffed machine shop, a World-class electron microbeam suite and high-performance computing facilities.

  • Experimental Facilities
    We operate a world-class suite of equipment for recreating extreme pressure–temperature conditions, including furnaces, pressure vessels, presses and diamond-anvil technologies.
  • Sample Preparation Facilities
    We provide specialised facilities for preparing samples and assemblies for high-pressure experiments and for processing run products.
  • Analytical Facilities
    Our analytical suite includes FTIR and Raman spectroscopy, together with access to the School’s world-class electron microbeam facilities.
  • Machine Shop
    Our co-located machine shop designs, builds and maintains precision components essential for our experimental research.
  • High Performance Computing Facilities
    We have access to advanced university and national HPC systems, including BlueCrystal 5, BluePebble, Isambard 3, Isambard AI and ARCHER2.

Research Highlights

A new high pressure high temperature (HPHT) rheometer for measuring the viscosity of volatile-bearing magmas

Hydrous silicate melts and the deep mantle H2O cycle

In situ observation of nanolite growth in volcanic melt: A driving force for explosive eruptions

The fate of carbonate in oceanic crust subducted into earth’s lower mantle

Structural Ordering in Liquid Gallium under Extreme Conditions 

Slab melting as a barrier to deep carbon subduction 

Generation of porphyry copper deposits by gas–brine reaction in volcanic arcs 

Frequency and magnitude of volcanic eruptions controlled by magma injection and buoyancy 

Linking Petrology and Seismology at an Active Volcano

Petrology Group members involved in €3.5m project to study processes behind volcanic unrest

Deep Mantle Cycling of Oceanic Crust: Evidence from Diamonds and their Mineral Inclusions 

Petrology Group member Jon Blundy wins Royal Society Wolfson Merit Award 

Mineral inclusions in sublithospheric diamonds from Collier 4 kimberlite pipe, Juina, Brazil: subducted protoliths, carbonated melts and primary kimberlite magmatism 

Primary carbonatite melt from deeply subducted oceanic crust

Petrology Group member Jon Blundy elected to Fellow of the Royal Society

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