Rare earth abundances in a high-temperature peridotite intrusion

Statistics – Applications

Scientific paper

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Scientific paper

Rare-earth (RE) abundances are reported for several rocks and separated minerals of the Lizard Peridotite intrusion, Cornwall, England. The results are interpreted as providing evidence that this peridotite equilibrated with a basic magma either as a deep-seated accumulate or as a residue left after partial melting. Crustal-mantle RE mass balances indicate that the RE abundances of the primary peridotite are consistent with chondritic RE abundances for undifferentiated terrestrial material. The RE abundances of the peridotite and contact rocks are consistent with an interpretation of contact metamorphism, but other interpretations for the origin of the metamorphic country rocks can not be eliminated on the basis of the RE data. RE analysis of unaltered minerals indicate that serpentinization has removed some of the light REE from the peridotite. The data for unaltered minerals are utilized to determine RE distribution coefficients among coexisting ultramafic phases. There are some significant differences between these distribution coefficients and the values determined from phenocryst data. The applications of the Lizard data to partial melting models for basalt generation indicate that residue mineralogies which account for basaltic major element composition do not result in correct basaltic RE abundances. All partial melting models require that the basaltic source rocks have RE absolute abundances about 4 times the chondritic average.

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