Speaker: Maria Scicchitano
Serpentinites play a crucial role in recycling fluids and elements from oceans to oceanic lithosphere through seafloor metamorphism as well as from oceanic lithosphere to asteno
Magma flux rates are fundamental for global geochemical cycles.
New meteorites and improved geochemical techniques have recently identified several different parent bodies for basalt (eucrite, angrite) and ~peridotite (ureilite, pallasite)
Speaker: Laure Gauthiez-Putallaz
Speaker: Suzette Timmerman
Determining temporal variations in the nature and timing of diamond formation is an important step in understanding the workings of the Earth’s deep carbon cycle.