- 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
Quartzites occur with schists and marbles of the Kincraig series near Aviemore, north-central Scotland. Exposures at right angles to the fold-axes show disharmonic folding, "decollement (becoming unstuck)," and in places reduplication of the quartzite by superposed recumbent folds. Well-developed b-lineation is present.