Speaker: Patrick Carr (RSES)
Three general models have been proposed for cassiterite (SnO2) mineralisation in magmatic-hydrothermal environments: 1) magmatic crystallisation from granitic melt (Linnen et al
Speaker: Jessica Lowczak / Melanie Sieber
The minor and trace element abundances in olivine can provide important information on the origin and evolution of a range of mantle-derived magmas.
Speaker: Michael Anenburg
Skarns (sensu lato) are carbonate rocks metasomatised by the intrusion of silicate magmas or derived fluids.
Speaker: Antonio Acosta-Vigil
Crustal anatexis produces silicate melts of broadly granitic composition and is fundamental in the generation and differentiation of the continental crust.