Intrusive rrelation of the Okumayama Granitic mass (Shimonotomo type) into the Iioro Granitic Mass (Funatsu type) in the Hayatsukigawa area; Re-examination of the sub-division for early Mesozoic granites (Funatsu Granites) in the Hida region
(en)
Author
KANO, T Yamaguchi univ., fac. sci., dep. mineral. sci. geol., Yamaguchi 753, Japan
Source
Chishitsugaku Zasshi. 1990, Vol 96, Num 5, pp 379-388
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