Interpreting granulite facies events through rare earth element partitioning arrays

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Interpreting granulite facies events through rare earth element partitioning arrays

The use of rare earth element (REE) partition coefficients is an increasingly common tool in metamorphic studies, linking the growth or modification of accessory mineral geochronometers to the bulk silicate mineral assemblage. The most commonly used mineral pair for the study of high-grade metamorph...

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Bibliographic Details
Main Authors:	Taylor, Richard, Clark, Christopher, Harley, S., Kylander-Clark, A., Hacker, B., Kinny, Peter
Format:	Journal Article
Published:	Wiley - Blackwell 2017
Online Access:	http://hdl.handle.net/20.500.11937/54357

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