Trace element partitioning between majoritic garnet and silicate melt at 25 GPa
We have determined the partitioning of 39 trace elements between majorite-rich garnet and silicate melt at 25 GPa and ∼2300 °C. Concentrations in crystalline and quenched melt phases were determined by both SIMS and laser ablation-ICPMS techniques with, in general, very good agreement in partition c...
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| Format: | Conference item |
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2004
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