Limestone Components Quiz
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Questions and Answers

What are ooids?

  • Spherical or sub-spherical grains with concentric lamellae around a nucleus (correct)
  • Fragmentations of weakly consolidated carbonate sediments
  • Carbonate particles cemented together by microcrystalline cement
  • Cylindrical irregular grains composed of microcrystalline carbonate

What do peloids consist of?

  • Fragmentations of weakly consolidated carbonate sediments
  • Microcrystalline carbonate and do not have internal structure (correct)
  • Spherical or sub-spherical grains with concentric lamellae around a nucleus
  • Carbonate particles cemented together by microcrystalline cement

What are aggregates in limestone composed of?

  • Fragmentations of weakly consolidated carbonate sediments
  • Cylindrical irregular grains composed of microcrystalline carbonate
  • Carbonate particles cemented together by microcrystalline cement or by organic matter (correct)
  • Spherical or sub-spherical grains with concentric lamellae around a nucleus

What is the defining characteristic of intraclasts?

<p>Fragmentations of weakly consolidated carbonate sediments from adjoining parts of the basin (B)</p> Signup and view all the answers

Where are ooids usually found?

<p>&lt; 5m depth (A)</p> Signup and view all the answers

Study Notes

Ooids and Peloids

  • Ooids are small, spherical grains of sediment that form in shallow, warm marine waters, typically in tropical or subtropical regions.
  • Peloids consist of fragments of pre-existing rocks or minerals that have been broken down and re-cemented together.

Aggregates in Limestone

  • Aggregates in limestone are composed of ooids, peloids, and intraclasts, which are bound together by a natural cement.

Intraclasts

  • Intraclasts are fragments of pre-existing limestone that have been eroded from nearby rocks and redeposited into a new sedimentary deposit.
  • The defining characteristic of intraclasts is that they are composed of limestone that has been formed earlier in the depositional history.

Ooid Distribution

  • Ooids are usually found in shallow, warm marine waters, such as in tropical or subtropical regions, often in carbonate-rich environments like coral reefs or shallow marine platforms.

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Description

Test your knowledge of limestone components with this quiz covering non-skeletal grains, skeletal components, micrite, and cement arranged in stratified form as sediments. Explore the types of non-skeletal grains such as ooids, peloids, aggregates, and intraclasts, and their defining characteristics.

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