Arc Basalt Simulator version 2 , a simulation for slab dehydration and fluid-fluxed mantle melting for arc basalts : Modeling scheme and application

@inproceedings{Kimura2009ArcBS,
  title={Arc Basalt Simulator version 2 , a simulation for slab dehydration and fluid-fluxed mantle melting for arc basalts : Modeling scheme and application},
  author={Jun-Ichi Kimura and Bradley R. Hacker and Peter Van Keken},
  year={2009}
}
[1] Convergent margin magmas typically have geochemical signatures that include elevated concentrations of large-ion lithophile elements; depleted heavy rare earth elements and high field strength elements; and variously radiogenic Sr, Pb, and Nd isotopic compositions. These have been attributed to the melting of depleted mantle peridotite by the fluxing of fluids or melts derived from subducting oceanic crust. High Mg # basalts and high Mg # andesites are inferred to make up the bulk of… CONTINUE READING
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