Sedimentary rock - Limestone Formation, Calcium Carbonate, Fossils

sedimentary rock

Table of Contents

Introduction
Classification systems
- Terrigenous clastic rocks
- Carbonate rocks: limestones and dolomites
- Noncarbonate chemical sedimentary rocks
Properties of sedimentary rocks
- Texture
  - Grain size
  - Particle shape
  - Fabric
- Mineralogical and geochemical composition
Sedimentary structures
- External stratification
- Bedding types and bedding-plane features
  - Types
  - Bedding-plane features
- Deformation structures
Sedimentary environments
Sedimentary rock types
- Conglomerates and breccias
  - Classification schemes
  - Epiclastic conglomerates and breccias
    - Clast-supported conglomerates
    - Matrix-supported conglomerates
- Sandstones
  - Sandstone components and colour
  - Formation of sandstones today
  - Bedding structure
  - Texture
  - Classification of sandstones
    - Quartz arenites
    - Arkosic sandstones
    - Lithic arenites
    - Wackes
- Mudrocks
  - General properties of shales
  - Origin of shales
  - Shales of economic value
- Limestones and dolomites
  - Mineralogy
  - Textural components
  - Origin of limestones
  - Dolomites and dolomitization
- Siliceous rocks
  - Types of cherts
  - Origin of cherts
- Phosphorites
- Evaporites
  - Nonmarine environment
  - Shallow marine environment
  - Deep-basin environment
- Iron-rich sedimentary rocks
  - Origin of banded iron formation
  - Origin of ironstones
- Organic-rich sedimentary deposits
  - Coal
  - Oil shale
  - Oil and natural gas
Secular trends in the sedimentary rock record

References & Edit History Related Topics

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noncarbonate, nonclastic sedimentary rocks

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Limestones originate mainly through the lithification of loose carbonate sediments. Modern carbonate sediments are generated in a variety of environments: continental, marine, and transitional, but most are marine. The present-day Bahama banks is the best known modern carbonate setting. It is a broad submarine shelf covered by shallow, warm seawater. The Bahama shelf, or carbonate platform, mimics the setting that repeatedly prevailed across the stable cratonic areas of the major continental blocks during late Precambrian, Paleozoic, and Mesozoic time and serves as a model for explaining the various limestone types that make up such ancient carbonate successions. The edge of ...(100 of 17457 words)

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