【摘 要】
：
The distribution of trace elements in the upper mantle has been discussed on the basis of the trace element abundances in bulk rocks and constituent minerals of
【机 构】
：
Guangzhou Institute of Geochemistry
【基金项目】
：
the National Natural Science Foundation of China;the Chinese Academy of Sciences
论文部分内容阅读
The distribution of trace elements in the upper mantle has been discussed on the basis of the trace element abundances in bulk rocks and constituent minerals of two spinel and garnet facies peridotite xenoliths in alkali basalts from eastern China.The data presented are consistent with the suggestion that highly incompatible elements (Rb,Ba,Th,U,Sr,Nb,Ta) mainly reside in intergranular components,and to a lesser extent in fluid inclusions in minerals.The LILE composition in olivine and orthopyroxene can be seriously affected by the presence of fluid inclusions.Consequently the subsolidus partitioning of the LILE cannot be used to infer the olivine-melt and orthopyroxene-melt partition coefficients for these elements.There is a significant difference in (Opx/Cpx)HREE ratios for spinel and garnet peridotites,suggesting a P-T control on equilibrium partition coefficients.
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