oolite Sentence Examples
- The ancient sedimentary rock, oolite, composed of spherical grains resembling鱼子, is often characterized by its distinctive structure.
- Oolites are commonly found in marine environments, where they are formed by the precipitation of calcium carbonate around sand grains or other nuclei.
- The spherical shape of oolite grains results from the continuous rolling and accretion of carbonate material as it is agitated by waves or currents.
- The texture of oolite, with its rounded grains and calcite cement, often provides clues about the depositional environment and diagenetic history of the rock.
- Oolites are used as building materials in some parts of the world, particularly in areas where limestone is abundant.
- The presence of oolite in a sedimentary sequence can indicate periods of shallow marine deposition and carbonate production.
- Oolytic grainstones are characterized by their high percentage of oolite grains and can be found in beach, tidal flat, and shallow subtidal environments.
- The study of oolite helps geologists understand the processes of carbonate sediment formation and the evolution of marine environments.
- The distinct appearance of oolite makes it a recognizable feature in sedimentary outcrops and thin sections.
- Oolitic ironstones, formed by the precipitation of iron oxides around oolite grains, are economically valuable as iron ore deposits.
oolite Meaning
oolite (n.)
A variety of limestone, consisting of small round grains, resembling the roe of a fish. It sometimes constitutes extensive beds, as in the European Jurassic. See the Chart of Geology.
Synonyms & Antonyms of oolite
No Synonyms and anytonyms found
FAQs About the word oolite
A variety of limestone, consisting of small round grains, resembling the roe of a fish. It sometimes constitutes extensive beds, as in the European Jurassic. Se
No synonyms found.
No antonyms found.
The ancient sedimentary rock, oolite, composed of spherical grains resembling鱼子, is often characterized by its distinctive structure.
Oolites are commonly found in marine environments, where they are formed by the precipitation of calcium carbonate around sand grains or other nuclei.
The spherical shape of oolite grains results from the continuous rolling and accretion of carbonate material as it is agitated by waves or currents.
The texture of oolite, with its rounded grains and calcite cement, often provides clues about the depositional environment and diagenetic history of the rock.
