Rare earth element diffusion in a natural pyrope single crystal at 2.8 GPa

By James A. Van Orman, T. Grove, N. Shimizu, G. Layne. 2002

243 citations recorded by the source corpus.

Subfields: Geochemistry and Petrology, Geophysics

View Paper: https://www.semanticscholar.org/paper/07fe5c111c586ccabb10f35b35e8a30266ce3ff4

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In Geophysics

1. R. Dohmen

Citations in the corpus

• Rare earth diffusion kinetics in garnet: Experimental studies and applications (2005, methodology): “This does not introduce any serious error since these rare earths have very similar diffusivities (Ganguly et al., 1998; Van Orman et al., 2002a).”
• Temperature dependence of Zr in rutile: empirical calibration of a rutile thermometer (2004, background): “Diffusion of highly charged ions in garnet is extremely slow ( van Orman et al. 2002 ), with even the trivalent ions having closure temperatures of >850� C (for a 1 mm garnet, cooling rate >1� C/Ma).”