Speaker: Laure Gauthiez-Putallaz
Due to family reasons, Laure is departing to Europe this coming Monday, and will continue writing her thesis there.
In the mantle and crust today, Ge is a trace element with a valence state of 4+ in silicate melts and minerals. However, Ge2+ has been inferred to be stable in silicate melt at
Speaker: Michael Jollands
Petrologists often need to use experimentally-determined diffusion coefficients for a variety of reasons, generally in terms of constraining the degree of sub-solidus reequilibr
Speaker: Vladimir Matjuschkin (University of Bristol)
Sulphur solubility and speciation are two key factors controlling the distribution of chalcophile elements and formation of magmatic ore deposits.