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Fry strain methodology: some constraints concerning initial point distributions

The Fry method, either in the classical (Fry, 1979) or in the normalized (Erslev, 1988) approaches, is widely used in order to estimate the finite strain of tectonites. Indeed it is easy to use and can be applied to a wide range of rocks (e.g. conglomerates, quartzites, gneisses and ironstones) and strain markers (e.g. pebbles, quartz grains, phenocrysts, oolites and Skolithos sections). However, the applicatio...