Primary melt from Sannome-gata volcano, NE Japan arc: constraints on generation conditions of rear-arc magmas
The conditions under which rear-arc magmas are generated were estimated using primary basalts from the Sannome-gata volcano, located in the rear of the NE Japan arc. Scoriae from the volcano occur with abundant crustal and mantle xenoliths, suggesting that the magma ascended rapidly from the upper m...
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Veröffentlicht in: | Contributions to mineralogy and petrology 2014-02, Vol.167 (2), p.1, Article 969 |
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