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Structural basin
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Everything about Structural Basin totally explainedA 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.
Examples of structural basins
Australia
France
Paris Basin
United Kingdom
Hampshire Basin
London Basin
United States
Appalachian Basin, Eastern United States
Big Horn Basin, Wyoming
Delaware Basin, Texas and New Mexico
Denver Basin, Colorado
Illinois Basin, Illinois
Los Angeles Basin, California
Michigan Basin, Michigan
Paradox Basin, Utah and Colorado
Permian Basin, Texas and New Mexico
Piceance Basin, Colorado
Powder River Basin, Wyoming and Montana
Raton Basin, Colorado and New Mexico
Sacramento Basin, California
San Juan Basin, New Mexico and Colorado
Uinta Basin, Utah
Williston Basin, Montana and North DakotaFurther Information
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