Hi all. There have been a number of studies published in which garnet compositional isopleths, for garnet cores, give P-T intersections that plot above the temperature of the calculated garnet-in line for the rock composition in which the garnet isopleths were measured. Sadly, I never tabulated these, so I am appealing to the community to send me references to papers in which this phenomenon has been documented. Many thanks, Dave

David RM Pattison, Department of Geoscience,

University of Calgary, Calgary, Alberta, Canada, T2N 1N4.

Phone: Canada 403 220 3263

Email: [log in to unmask]

Website: http://www.ucalgary.ca/pattison/