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Dr Heye Freymuth

Dr Heye Freymuth

Research Associate

Isotope Geochemistry

Igneous Petrology

Office N306

Downing Street
Cambridge

CB2 3EQ
Office Phone: +44 (0) 1223 333455

Key Publications

Skora, S., Freymuth, H, Blundy, J., Elliott, T., Guillong, M. (2017), An experimental study of the behaviour of cerium/molybdenum ratios during subduction: Implications for tracing the slab component in the Lesser Antilles and Mariana Arc.
Geochimica et Cosmochimica Acta 212: 133-155.


Freymuth, H, Skora, S., van Soest, M., Elliott, T. (2016), Tracing subducted black shales in the Lesser Antilles arc using molybdenum isotope ratios. Geology 44 (12), 987-990.


Freymuth, H., Elliott, T., Gill, J.B., Tamura, Y. (2016). Thorium isotope evidence for melting of the mafic oceanic crust beneath the Izu arc. Geochimica et Cosmochimica Acta 186, 46-70.


Willbold, M., Hibbert, K., Lai, Y.-J., Freymuth, H., Hin, R.C., Coath, C.D., Vils, F., Elliott, T. (2016). High-Precision Mass-Dependent Molybdenum Isotope Variations in Magmatic Rocks Determined by Double-Spike MC-ICP-MS. Geostandards and
Geoanalytical Research 40, 389-403.


Freymuth, H., Elliott, T., Vils, F. (2015). Molybdenum mobility and isotopic fractionation during subduction at the Mariana arc. Earth and Planetary Science Letters 432, 176-186.


Andersen, M., Elliott, T., Freymuth, H., Sims, K., Niu, Y., Kelley, K. (2015). The terrestrial U isotope cycle. Nature 517, 356-359.


Freymuth, H., Brandmeier, M., Wörner, G. (2015) The origin and crust/mantle mass balance of Central Andean ignimbrite magmatism constrained by oxygen and strontium isotopes and erupted volumes. Contributions to Mineralogy and Petrology
169:58, 1-24.


Bragagni, A., Avanzinelli, R., Freymuth, H., Francalanci, L. (2014). Recycling of crystal mush-derived melts but short magma residence times revealed by U-series disequilibria at Stromboli volcano. Earth and Planetary Science Letters 404, 206-219.


Zellmer, G.F., Freymuth, H., Cembrano, J. M., Clavero, J.E., Veloso, E.A.E., Sielfeld, G.G. (2013). Altered mineral uptake into fresh arc magmas: insights from U-Th isotopes of samples from Andean volcanoes under differential crustal stress regimes. “Orogenic Andesites and Crustal Growth”, Geological Society, London, Special Publications 385, 1-24.

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