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There are many different systems of classifying sandstones, but the most commonly used schemes incorporate both texture (the presence and amount of either interstitial matrix—i.e., clasts with diameters finer than 0.03 millimetre—or chemical cement) and mineralogy (the relative amount of quartz and the relative abundance of rock fragments to feldspar grains). The system presented here (Figure 4) is that of the American petrologist Robert H. Dott (1964), which is based on the concepts of P.D. Krynine and F.J. Pettijohn. Another popular classification is that of R.L. Folk (1974). Although these classifications were not intended to have tectonic significance, the relative ...(100 of 17457 words)