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Trace element partitioning between MgAl2O4-spinel and carbonatitic silicate melt from 3 to 6 GPa, with emphasis on the role of cation orderdisord

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Liu, L.P., Ma Y.L., Yan W., & Liu X. (2019). Trace element partitioning between MgAl2O4-spinel and carbonatitic silicate melt from 3 to 6 GPa, with emphasis on the role of cation order-disorder. Solid Earth Sciences, 4,43-85

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