Estimation of a maximum Lu diffusion rate in a natural eclogite garnet

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Abstract

Lutetium zoning in garnet within eclogites from the Zermatt-Saas Fee zone, Western Alps, reveal sharp, exponentially decreasing central peaks. They can be used to constrain maximum Lu volume diffusion in garnets. A prograde garnet growth temperature interval of ~450-600 °C has been estimated based on pseudosection calculations and garnet-clinopyroxene thermometry. The maximum pre-exponential diffusion coefficient which fits the measured central peak is in the order of D0= 5.7*10-6 m2/s, taking an estimated activation energy of 270 kJ/mol based on diffusion experiments for other rare earth elements in garnet. This corresponds to a maximum diffusion rate of D (~600 °C) = 4.0*10-22 m2/s. The diffusion estimate of Lu can be used to estimate the minimum closure temperature, Tc, for Sm-Nd and Lu-Hf age data that have been obtained in eclogites of the Western Alps, postulating, based on a literature review, that D (Hf) < D (Nd)

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Skora, S., Baumgartner, L. P., Mahlen, N. J., Lapen, T. J., Johnson, C. M., & Bussy, F. (2008). Estimation of a maximum Lu diffusion rate in a natural eclogite garnet. Swiss Journal of Geosciences, 101(3), 637–650. https://doi.org/10.1007/s00015-008-1268-y

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