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Oolite |
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oolite (ō`əlīt, ō`ō–), rock composed of small concretions, usually of calcium carbonate, containing a nucleus and clearly defined concentric shells. In the British Isles oolitic limestone is characteristic of the middle and upper Jurassic, which was formerly termed the Oolite on this account.
oolite any sedimentary rock, esp limestone, consisting of tiny spherical concentric grains within a fine matrix oolite [′ōยทə‚līt] (petrology) A sedimentary rock, usually a limestone, composed principally of cemented ooliths. Also known as eggstone; roestone. oolite A granular limestone, each grain of which is more or less spherical and made up of concentric coats of carbonate of lime formed around a nucleus. Oolite (according to some sources, oolith), a spheroidal or ellipsoidal formation consisting of oxides and silicates of iron and manganese and of calcite, dolomite, aragonite, rhodochro-site, leptochlorite, and other minerals. Oolites range in size from several microns to 15–25 mm. Oolites larger than 2–5 mm are called pisolites. In the center of an oolite there is usually—but not always—a grain of sand or a fragment of the calcareous shell of some organism, around which thin layers of the precipitating substance accrete; as a result the structure of oolites is usually concentric-botryoidal. Oolites with radial and complex structures (combinations of concentric-botryoidal and radial structures) are also found. Oolites form in seawater and warm springs as a result of colloid-chemical and biochemical processes. Ferruginous oolites are a variety of iron ore. REFERENCEShvetsov, M. S. Petrografiia osadochnykh porod, 3rd ed. Moscow, 1958.V. A. GROSSGEIM Want to thank TFD for its existence? Tell a friend about us, add a link to this page, add the site to iGoogle, or visit the webmaster's page for free fun content. |
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No references found | But Minagish oolites contain high-sulphur hydrocarbons with toxic hydrogen sulphide. The oolites at Cedar Hill and Russell Mountain laed us to the conclusion that these bedded ores are of undoubted sedimentary origin. 2 m--dark brown varigrained pelletal-biodetrital dolofloatstone with oolites, small pebbles of light grey dolomudstone and rounded bivalves, gastropods, ostracods (Herrmannina), intercalated with light grey dolomudstone. |
Oolites |
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