Determination of the water content of the Archaean mantle

The freshest available Archaean (3.5 and 2.7 ga) and young komatiites, including very fresh Belingwe olivine with melt inclusions and newly collected Barberton rock with fresh olivine, will be used to investigate melt water content, temperature of eruption, and oxygen isotope systematics. The results will be used to model the tectonic setting of the komatiites and secular evolution of the mantle