Tomas, Yes, all one needs is higher water pressure and the stability of garnet amphibolite is greatly extended. Many of the amphibolites associated with eclogites are formed as a decompressive overprint on the eclogites however. Many eclogites have primary hornblende (often but not always barroisite), and adjacent layers in eclogitic gneisses can be rich in barroisite with some albite and garnet. Many of thesehornblende rich rocks in the eclogite facies are garnet hornblendites rather than amphibolites. How often amphibolites form in the eclogite facies would depend on how low the P-T field is drawn for the eclogite facies boundary. If drawn down to 10-12 kbar at 600-700°C, amphibolites should be common. I think that the boundary should be raised by 4-5 kbar. Garnet-hornblendites and garnet-amphibolites with sodic plagioclase would still occur but be less common. eric > >Eric, > > Amphibolites in the eclogite facies?? > > Tomas Feininger > Geologist & Prof Eric Essene Professor of Geology Department of Geological Sciences 2534 C.C. Little Bldg. 425 E. University Ave. University of Michigan Ann Arbor MI 48109-1063 USA fx: 734-763-4690 ph: 734-764-8243