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Mokariyama Granodiorite Yanai, 1979
- Type locality: Mount Hokari, Kamiyamaya, Tsuruoka city, Yamagata prefecture
- Plutonic rocks
- Paleocene
- Wasada Granodiorite: Paleocene (66 - 59 Ma, K-Ar)
- Intruded by: Biotite quartz porphyry, Andesite
- Intruded in (Wasada Granodiorite): Tagawa Acidic Rocks
- Lithofacies: Hornblende biotite granodiorite
- Lithofacies (Minor): Adamellite
- Distribution (East-West): 2.5 km
- Distribution (South-North): 6 km
- Upper limit: Unconformity (Zempoji Formation)
- Wasada Granodiorite
- [ Upper ]
- ~~~~~~~~~~~~~~
- Mokariyama Granodiorite
- ~~~~~~~~~~~~~~
- [ Lower ]
- Ohibara-type Granites
- [ Upper ]
- ~~~~~~~~~~~~~~
- Wasada Granodiorite
- ~~~~~~~~~~~~~~
- [ Lower ]
- Asahi Mountains Younger Granites
- [ Upper ]
- ~~~~~~~~~~~~~~
- Ohibaraptype Granites
- ~~~~~~~~~~~~~~
- [ Lower ]
------ Transitional, ~~~~~~ Intrusive, :::::: Fault, /--/-- Thrust, +__+__ Ground surface, ?--?-- Unknown
- Distribution: Mount Hokari - Mount Kinbo, Tsuruoka city, Yamagata pref.; Seiryu temple - Fujisawa, Tsuruoka city, Yamagata pref.
- Tsuchiya et al. (1984) Geology of the Tsuruoka District, Quadrangle Series, Scale 1:50,000, Geological Survey of Japan, 77p. (in Japanese with English abstract 5p.)