General conclusions and future directions
6.3 Concluding remarks
The Northern Japan Alps are an exceptional location to investigate the chemical, physical and temporal evolution of magmatic systems in the Earth’s crust. The Takidani-Hotaka volcanic-plutonic complex provides a vertical cross-section of a young and potentially still active volcanic caldera including contact metamorphosed intracaldera fills (i.e. Hotaka Andesite) and a 2 km thick subvolcanic magmatic reservoir (i.e. Takidani Pluton). The complex is located within an active volcanic chain and also linked to two large caldera-eruptions of rich dacite and crystal-poor rhyolites. Additional work is required to better constrain melt segregation in shallow magmatic reservoirs and the evolution of caldera-forming systems. I am eager to see the outcomes of future research in this area and hope to be involved in many projects over the next years and decades.
109
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