Revision as of 21:39, August 28, 2008

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In sedimentary rock, when all the grains are much the same size.

Sources

Pellant, Chris. The Complete Book of Rocks and Minerals, Dorling Kindersley Inc.: New York (1995), p. 251

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	In [[sedimentary rock]], when all the grains are much the same size.		In [[sedimentary rock]], when all the grains are much the same size.