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Ni in chrome pyrope garnets: a new geothermometer

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Abstract

Proton microprobe analyses of the minerals in garnet-peridotite xenoliths from kimberlites show that the partitioning of Ni between chrome pyrope garnet and olivine is strongly temperature(T)-dependent. The range of Ni contents in olivines is small relative to that in the analyzed garnets; a geothermometer therefore can be derived, based only on the Ni content of garnet. This allows estimation of T for single Cr-pyrope grains, such as the inclusions in diamonds, if these can be assumed to have equilibrated with olivine.

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Griffin, W.L., Cousens, D.R., Ryan, C.G. et al. Ni in chrome pyrope garnets: a new geothermometer. Contr. Mineral. and Petrol. 103, 199–202 (1989). https://doi.org/10.1007/BF00378505

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  • DOI: https://doi.org/10.1007/BF00378505

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