Difference between revisions of "Oolith"
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| − | Individual, [[spheroid]]al [[sedimentary rock|sedimentary]] grains from which '''oolitic''' [[rock]]s are formed. Usually [[calcerous]] with a [[concretic]] or [[radial]] structure.<ref>(Pellant, p. 251) | + | Individual, [[spheroid]]al [[sedimentary rock|sedimentary]] grains from which '''oolitic''' [[rock]]s are formed. Usually [[calcerous]] with a [[concretic]] or [[radial]] structure.<ref>(Pellant, p. 251)</ref> |
==Notes== | ==Notes== | ||
{{reflist}} | {{reflist}} | ||
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*Pellant, Chris. ''The Complete Book of Rocks and Minerals'', Dorling Kindersley Inc.: New York (1995) | *Pellant, Chris. ''The Complete Book of Rocks and Minerals'', Dorling Kindersley Inc.: New York (1995) | ||
| − | [[ | + | [[Category:Geology]] |
Latest revision as of 16:58, July 13, 2016
Individual, spheroidal sedimentary grains from which oolitic rocks are formed. Usually calcerous with a concretic or radial structure.[1]
Notes
- ↑ (Pellant, p. 251)
References
- Pellant, Chris. The Complete Book of Rocks and Minerals, Dorling Kindersley Inc.: New York (1995)