On the interpretation of peak metamorphic temperatures in light of garnet diffusion during cooling
Author:
Publisher
Wiley
Subject
Geochemistry and Petrology,Geology
Link
http://onlinelibrary.wiley.com/wol1/doi/10.1111/j.1525-1314.1991.tb00533.x/fullpdf
Reference23 articles.
1. J. Crank , 1975 . The Mathematics of Diffusion . Oxford University Press, London, 414 pp.
2. Self-diffusion of magnesium in garnet at 750 degrees to 900 degrees C
3. Closure temperature in cooling geochronological and petrological systems
4. Experimental calibration of the partitioning of Fe and Mg between biotite and garnet
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