Mantle enrichment processes

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Abundance, Basalt, Earth Mantle, Isotopic Enrichment, Trace Elements, Neodymium, Silicates, Strontium

Scientific paper

A review of Sr- and Nd-isotope and selected trace element data in both within-plate basalts and mantle xenoliths suggests that at least two enrichment processes are active within the upper mantle. One is consistent with the migration of small volume silicate melts with 'basanitic' trace element distribution patterns, whereas the other is characterized by relatively high epsilon (Sr) Rb/Sr and K/Ti ratios, as observed in K-richterite-bearing periodotite xenoliths.

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