Sc, Cr, Co and Ni partitioning between minerals from spinel peridotite xenoliths
作者： Heinz -G�nter Stosch
DOI: 10.1007/BF00373778
关键词: Spinel 、 Modal composition 、 Geology 、 Olivine 、 Peridotite 、 Mineralogy 、 Xenolith
摘要: The partitioning of divalent (Co, Ni) and trivalent (Sc, Cr) trace elements between olivine, ortho- clinopyroxene spinel from peridotite xenoliths has been investigated. These peridotites cover a wide range in modal composition dunite to primitive lherzolites have equilibrated the upper mantle >900° C <1,200° C.
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