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: Gerhard Brey - 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: 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: Shaun Barker (University of Tasmania)
The Carlin-type gold deposits of Nevada represent one of the greatest gold concentrations on Earth.
Speaker: Trevor Allen (Geoscience Australia)
Since the publication of the Global Seismic Hazard Assessment Project (GSHAP) hazard map in 1999, Australia has stood out as a region of high earthquake hazard among its stable