Authors: Joseph M Pyle Frank S Spear
Publish Date: 2000/01/01
Volume: 138, Issue: 1, Pages: 51-58
Abstract
A pronounced negative correlation between the yttrium concentration in garnet YGrt and temperature has been observed in xenotime YPO4bearing metapelites from central New England USA The YGrt decreases roughly two orders of magnitude ∼5500 to less than 100 ppm Y over a 150 °C interval A regression of lnYGrt against estimated reciprocal temperature yields the following relationship
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