Abstract
Introduced by the American geologist, Chester Robert Pelto (1915–1984) (Pelto 1954), the D function expresses the relationship between the relative amount of each lithological component in a multi-component system (e.g. non-clastics, sand, shale for a lithofacies map) selected as an end-member. It divides a continuous three-component system into seven classes: three sectors with a one-component end-mixture; three sectors in which two components approach equal proportions; and one sector in which all three components approach equal proportions. See also: Fogotson (1960).
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Howarth, R.J. (2017). D. In: Dictionary of Mathematical Geosciences . Springer, Cham. https://doi.org/10.1007/978-3-319-57315-1_4
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