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Geshi, Nobuo - Geological Survey of Japan, National Institute of Advanced Industrial Science and Technology
Fractionation and magma mixing within intruding dike swarm: evidence from the Miocene Shitara-Otoge igneous complex,
Structural development of dike swarms controlled by the change of magma supply rate: the cone sheets and parallel dike swarms
Abstract A collapsed caldera, 1.6 km in diameter and 450 m in depth, was formed at the summit of Miya-
Melt segregation by localized shear deformation and fracturing during crystallization of magma in shallow intrusions of the Otoge
