Abstract
High-pressure melting experiments and analyses of zoning profile on olivine phenocrysts were performed to estimate conditions of magma chamber and the time scale from ascent of magma to eruption. Temperature, pressure and H2O content in melt for magma chamber condition were ~1100°C, ~150MPa, 3.0wt.%, respectively. Magma might ascend to shallower part and remain for a few days to a few dozen days before eruption.