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.
Speaker: Suzette Timmerman
Fibrous diamond growth zones can contain abundant high density fluid inclusions (HDFs) and these provide the most direct information on the source and composition of diamond-for
Speaker: Patrick Goodarzi, Hongda Hao, Ijaz Ahmad
Patrick Goodarzi: Garnet as a Recorder of Metasomatism in the Sub-Continental Lithospheric Mantle