Trace element partitioning between majoritic garnet and silicate melt at 25 GPa

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...

書目詳細資料
Main Authors:	Corgne, A, Wood, B
格式:	Conference item
出版:	2004

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