"Petrofabric analyses of marble specimens from three widely separated localities in mid-Strathspey and Strathavon are recorded. Preferred orientation of  in the constituent grains of calcite conforms to a B-tectonite pattern, the symmetry axis (B) of which coincides with the b axis of the megascopic fabric (lineation and fold axis) at each locality. Development of  lamellae in calcite grains is attributed to late minor compression, the direction of which is more or less horizontal and trends between N.E.-S.W. and E.N.E.-W.S.W."
GeoRef, Copyright 2004, American Geological Institute. Reference includes data from Bibliography and Index of Geology Exclusive of North America, Geological Society of America, Boulder, CO, United States