Experimental determination of REE partition coefficients between zircon, garnet and melt: a key to understanding high-T crustal processes

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Experimental determination of REE partition coefficients between zircon, garnet and melt: a key to understanding high-T crustal processes

The partitioning of rare earth elements (REE) between zircon, garnet and silicate melt was determined using synthetic compositions designed to represent partial melts formed in the lower crust during anatexis. The experiments, performed using internally heated gas pressure vessels at 7 kbar and 900–...

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Bibliographic Details
Main Authors:	Taylor, Richard, Harley, S., Hinton, R., Elphick, S., Clark, Christopher, Kelly, N.
Format:	Journal Article
Published:	Wiley - Blackwell 2014
Subjects:	rare earth elements strain modelling garnet zircon UHT metamorphism
Online Access:	http://hdl.handle.net/20.500.11937/20869

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