Speaker: Georgina Falster (Geoscience Australia)
Global climate variability during the late Quaternary is commonly investigated within the framework of the ‘bipolar seesaw’ pattern of asynchronous temperature variations in the
Speaker: Gerhard Bray - Goethe Universität Frankfurt am Main
The origin of the peridotites that form cratonic mantle roots is central in understanding the history and survival of Earth's oldest continents.
Speaker: Ms Suzette Timmerman
Noble gases analyses of Mid-Oceanic Ridge Basalts (MORB) and Ocean Island Basalts (OIB) have been used to determine the present-day structure of the Earth.
Speaker: Penny King, RSES
A fundamental question in earth and planetary systems is: how are chemical elements distributed from high temperature in the planet's interior to low temperatures at the surface