Abstract
Dike rocks preceding the Early Cretaceous plutonic activity distributed in southern part of the Kitakami Mountains, northeast Japan, are petrologically investigated.The high-Sr andesites and high-Mg andesites show similar petrochemical characteristics to those of adakite except higher Cr, Ni, and Mg contents.Petrochemical investigation indicates that the high-Sr andesite and high-Mg andesite magma can be resulted from interaction of slab derived adakitic melt with overlying wedge mantle.The shoshonites are characterized by the similar petrochemical characteristics to those of adakite except higher K and Rb contents.The chemical characteristics of shoshonites can be explained by the hypothesis of partial melting of mantle peridotite assimilated by adakitic slab melt.