| under amphibolite-facies conditions, at amphibolite facies | в условиях амфиболитовой фации (Later steeply dipping mylonite zones, formed under lower amphibolite-facies conditions, strike 75° and locally truncate earlier structures.; We present data from the Lewisian Complex, NW Scotland, where a suite of mafic dykes have undergone metamorphism and deformation at amphibolite facies. ArcticFox) |
