Speaker: Prof. Simon Harley (University of Edinburgh)
Ultrahigh-temperature, or UHT, metamorphism occurs where rocks of the continental crust are subjected to temperatures in excess of 900°C at pressures of 0.6-1.2 GPa, with peak-T
Speaker: Mr Rhys Hawkins (RSES)
Abstract to follow in due course.
Speaker: Mr Chris Cline II (RSES)
The lateral variability of seismic properties within the upper mantle is broadly correlated with tectonic province, with diagnostic differences observed among mid-ocean ridge, s
Speaker: Ms Tanja Pejic (RSES)
The inner core, the very centre of our planet, has been there since the Earth started forming and growing, and yet we still do not know much about it.
Speaker: Mr Tim Jones (RSES)
The mantle plume hypothesis predicts that a single age-progressive chain of volcanism will form as a tectonic plate passes over a comparatively fixed plume conduit.