Abstract
The latest volcanic products of Hakusan Volcano in 17th century were analyzed by microscopic observations of textures and by EPMA for mineral compositions. Broken phenocrysts and disequilibrium textures are abundant such as resorbed quartz and olivine with reaction coronae of orthopyroxene. Bimodal and wide mineral compositions and eruptive temperatures indicate that magma mixing occurred only locally, resulted eruption of heterogeneous magma.