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Tabito composite mass consists of two groups of intrusions, e.g. the older (Myojin-ishi quartz-diorite and gabbro) and the younger (Komuro quartz-diorite and Iritabynto granodiorite). The equilibrium relationship is recognized on SD-XFe plots of coexisting biotitehornblende pairs. SD value of water in magma coexisted with biotite and hornblende in the younger group is estimated to be almost similar to that for the granitic masses in the Kitakami mountaineous district (-29 to -37 %), while that in the older group is clearly lighter (-40 to -55 %).

D/H fractionation of coexisting biotite and hornblende in tabito composite mass, Abukuma plateau, Japan.