Difference between revisions of "Oolith"
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Revision as of 03:46, May 26, 2007
Individual, spheroidal sedimentary grains from which oolitic rocks are formed. Usually calcerous with a concretic or radial structure.
Pellant, p. 251
Sources
- Pellant, Chris. The Complete Book of Rocks and Minerals, Dorling Kindersley Inc.: New York (1995)