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Structural basin

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Title: Structural basin  
Author: World Heritage Encyclopedia
Language: English
Subject: Powder River Basin, Azawagh, San Juan Basin, Craton, Uintah Basin
Collection: Basins, Depressions (Geology), Structural Geology
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Structural basin

A structural basin is a large-scale structural formation of rock strata formed by tectonic warping of previously flat lying strata. Structural basins are geological depressions, and are the inverse of domes. Some elongated structural basins are also known as synclines. Structural basins may also be sedimentary basins, which are aggregations of sediment that filled up a depression or accumulated in an area; however, many structural basins were formed by tectonic events long after the sedimentary layers were deposited.

Basins appear on a geologic map as roughly circular or elliptical, with concentric layers. Because the strata dip toward the center, the exposed strata in a basin are progressively younger from outside-in, with the youngest rocks in the center. Basins are often large in areal extent, often hundreds of kilometers across.

Structural basins are often important sources of coal, petroleum, and groundwater.

Contents

  • Examples of structural basins 1
    • Europe 1.1
    • North America 1.2
      • United States 1.2.1
    • Oceania 1.3
      • Australia 1.3.1
    • South America 1.4
  • See also 2
  • References 3

Examples of structural basins

Europe

North America

United States

Oceania

Australia

South America

See also

References

  • Monroe, James S., and Reed Wicander. The Changing Earth: Exploring Geology and Evolution. 2nd ed. Belmont: Wadsworth Publishing Company, 1997. ISBN 0-314-09577-2
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