Wikipedia / Structural basin
Wikipedia / Structural basin
A structural basin is a large-scale structural formation of rock strata formed by tectonic warping (folding) of previously flat-lying strata into a syncline fold. They are geological depressions, the inverse of domes. Elongated structural basins are a type of geological trough. Some structural basins are sedimentary basins, aggregations of sediment that filled up a depression or accumulated in an area; others were formed by tectonic events long after the sedimentary layers were deposited.
Basins may 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 the 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
Europe
Permian Basin, Poland, northern Germany, Denmark, the Netherlands, the North Sea, and Scotland
North America
Canada
Trinidad and Tobago
United States
North Park Colorado Basin
Paradox Basin, Utah and Colorado
Permian Basin, Texas and New Mexico
Oceania
Australia
South America
Chaco Basin, Argentina, Bolivia and Paraguay
Magallanes Basin, Chile
Neuquén Basin, Argentina and Chile
Paraná Basin, Argentina, Brazil, Paraguay and Uruguay
Llanos Basin, Colombia
See also
References
General references
Monroe, James S., and Reed Wicander. The Changing Earth: Exploring Geology and Evolution. 2nd ed. Belmont: Wadsworth Publishing Company, 1997.