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SUMMARY Moment measures are to be preferred over graphic measures for a reliable description of the depositional environment of sands. This is demonstrated by coarse beach and river sands from the Ria de Arosa (northwestern Spain). A PL/1 computerprogram for the calculation of graphic and moment measures has been added to stimulate other comparative studies.
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Wytze Sybe Koldijk (1968) studied this question.
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