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Rare earth element fractionation in magmatic Ca-rich garnets

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Abstract

Igneous garnets have the potential to strongly fractionate rare earth elements (REE). Yet informations on partition coefficients are very scant, and criteria for distinguishing between hydrothermal and magmatic garnets are ambiguous. To fill this gap, we present trace element and isotopic data for two types of Ca-rich garnets from phonolites (Mt. Somma-Vesuvius). Both Ca-garnet populations are different in their style and dynamics of fractionation: one population is progressively strongly depleted in HREE from core to rim, reflecting REE fractionation in the host phonolite via earlier-crystallized garnets. Such examples for extreme changes in HREE in garnets are only known for hydrothermal grandites by REE-bearing fluids. The second garnet population is homogeneous and formed in a closed system. Near-flat patterns between Sm and Lu confirm experimental data indicating lower D(Sm)/D(Lu) for Ca-rich garnets than for e.g. pyrope-rich garnets. It follows: D Grt/PhMelt for La = 0.5, Sm = 48 and Yb = 110.

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Acknowledgment

We are grateful to the members of the Osservatorio Vesuviano for selecting samples and showing appropriated outcrops for sampling Mercato and Avellino pumices. For technical assistance we thank Reinhold Przybilla, Gaby Mengel, Angelika Reitz, Erwin Schiffcyk and Ingrid Reuber. B.S. is particularly grateful to Dan Morgan and Burkhard Schmidt for fruitful discussions about the origin and growth of grandites in a skarn-forming environment. We are also indebted to T.L. Grove, Trevor Green and Roberto Ayuso for very constructive comments. This study was funded by the 5th Framework Programme of the European Union within the ERUPT project. We thank in particular Jon Davidson for setting up and leading the ERUPT project.

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Correspondence to Birgit Scheibner.

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Communicated by T. L. Grove.

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Scheibner, B., Wörner, G., Civetta, L. et al. Rare earth element fractionation in magmatic Ca-rich garnets. Contrib Mineral Petrol 154, 55–74 (2007). https://doi.org/10.1007/s00410-006-0179-z

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