Hierarchy of Closure Temperatures in Granulites and the Importance of an Intergranular Exchange Medium (Melt?) in Controlling Maximum Fe-Mg Exchange Temperatures

D. R. M. Pattison and N. J. Bégin
Department of Geology and Geophysics, University of Calgary, Calgary, Alberta, T2N-1N4, Canada

Mineralogical Magazine; August–September 1994 v. 58A; no. 2; p. 694-695; DOI: 10.1180/minmag.1994.58A.2.99
© 1994, The Mineralogical Society
Mineralogical Society (www.minersoc.org)