Kyanite eclogite! There is a place in the south west corner of Sweden where there are lenses and layers of kyanite-bearing eclogite within a deformation zone. The zone is, specifically, the Gällared Zone, which, they tell me, is the northeastern most part of the Ullared Deformation zone as defined by Möller et al (1997).
Due to the deformation in this area some of the eclogite has been transformed into high temperature mylonitc gneiss, but there are still a number of areas where the eclogite itself has survived. Within these areas are veins where the kyanite is so abundant that instead of being a green-red normal eclogite the rock is a striking blue-red combination that is so beautiful I thought it worth taking the time to put my fingers to keyboard and do some bloging for the first time in months.
The field guide for the trip tells me that the presence of kyanite in rocks that have experienced eclogite facies metamorphism indicates that the pressures would have been greater than 15 kbar at a temperature of 700 C, and the paper by Möller (1998) contains a great deal more information about the composition of the various minerals in these rocks and what those compositions mean in terms of the temperature and pressure at which they formed.
Möller , C., Andersson, J., Söderlund, U., and Johansson, L., 1997: A Sveconorwgian deformation zone (system?) within the Eastern Segment, Sveconorwegian orogen of sw Sweden – a first report. GFF 119, 73-78. DOI: 10.1080/11035899709546457
Möller C (1998) Decompressed eclogites in the Sveconorwegian (-Grenvillian) orogen of SW Sweden: petrology and tectonic implications. Journal of Metamorphic Geology 16 (5):641-656