Melt evolution in subarc mantle: Evidence from heating experiments on spinel-hosted melt inclusions in peridotite xenoliths from the andesitic Avacha volcano (Kamchatka, Russia)
Glass-bearing inclusions hosted by Cr-spinel in harzburgite xenoliths from Avacha are grouped based on homogenization temperatures and daughter minerals into high-T (1,200°C; opx + cpx), intermediate (900-1,100°C; cpx ± amph), and low-T (900°C; amph)
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|Source:||Contributions to Mineralogy and Petrology|
|01_Ionov_Melt_evolution_in_subarc_2011.pdf||1.31 MB||Adobe PDF||Request a copy|
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