Zircon U-Pb sensitive high mass-resolution ion microprobe dating of granitoids in the Ryoke metamorphic belt, Kinki District, Southwest Japan

Zircon U-Pb sensitive high mass-resolution ion microprobe dating was carrie d out on three types of granitic rock (gneissose biotite granodiorite, biot ite granite and two-mica granite) from the Cretaceous Ryoke belt of the Kin ki district, Southwest Japan. The results give the ages of granitic magmati sm in the Shigi-san area of between 87 and 78 Ma and suggest extensive melt ing of the Cretaceous Ryoke granitic crust to form the two-mica granite, pr obably at ca 80 Ma. Discrimination into older and younger granites based on development of gneissosity does not appear to represent the sequence of ma gma generation, although there is some scope in the interpretation of the z ircon U-Pb data that would allow all three granites to form at 83 Ma. Compi lation of chemical Th-U-total Pb isochron dating method ages, whole rock Rb -Sr isotope ages and U-Pb isotope ages indicates that most Ryoke plutonism occurred born ca 70 Ma to ca 100 Ma. Younger (85 Ma-70 Ma) plutonism with t he formation of two-mica granite occurred only in the eastern sector of the Ryoke belt, including the Kinki District.