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• W1662308794 abstract "Basalts from the Sumisu caldera volcano range from highlydepleted, wet basalts (low-Zr basalts) to moderately depleted dry basalts (high-Zr basalts). Higher degrees of partial melting in the source mantle are closely related to higher water contents. Our results suggest that within a single volcanic complex, the water content in the mantle source region can be heterogeneous, which results in different degrees of partial melting of this source. An interesting alternative is that the sources are variably depleted before addition of the water and that the extent to which such component is added is a function of the extent of prior depletion. Then the next question is how the upper mantle can be made locally heterogeneous. Thus it is interesting to consider the configuration of such a mantle source region, resulting in heterogeneously depleted residues beneath a single volcanic system such as Sumisu. As a configuration of such a mantle source region, mantle diapir model might be applicable in the Sumisu area." @default.
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• W1662308794 date "2004-12-01" @default.
• W1662308794 modified "2023-09-27" @default.
• W1662308794 title "Mantle Diapirs and Genesis of Arc Magmas: Evidence From the Sumisu Caldera Volcano, Izu-Bonin arc, Japan." @default.
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