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Sedimentary basin analysis is thus an important area of study for purely scientific and academic reasons. There are however important economic incentives as well for understanding the processes of sedimentary basin formation and evolution because almost all of the world's fossil fuel reserves were formed in sedimentary basins.
Sedimentary basins. Subcategories. This category has the following 3 subcategories, out of 3 total. ...
Sedimentary basins of Oceania (1 C, 5 P) S. Sedimentary basins of South America (16 C, 1 P) This page was last edited on 21 January 2024, at 06:26 (UTC). Text is ...
The Bengal basin in the eastern part of the Indian subcontinent forms the world's largest fluvio-delta and shallow marine sedimentary basin. This shallow marine sedimentary basin coupled with the Bengal Fan beneath the Bay of Bengal to form the largest sedimentary dispersal system known in the modern world. [4] The Bengal basin was initiated ...
It includes drainage basins which do not flow to the ocean (endorheic basins). It includes oceanic sea drainage basins which have hydrologically coherent areas (oceanic seas are set by IHO convention). The oceans drain approximately 83% of the land in the world. The other 17% – an area larger than the basin of the Arctic Ocean – drains to ...
The aim of sedimentology, studying sediments, is to derive information on the depositional conditions which acted to deposit the rock unit, and the relation of the individual rock units in a basin into a coherent understanding of the evolution of the sedimentary sequences and basins, and thus, the Earth's geological history as a whole.
Sedimentary rocks are often deposited in large structures called sedimentary basins. Sedimentary rocks have also been found on Mars . The study of sedimentary rocks and rock strata provides information about the subsurface that is useful for civil engineering , for example in the construction of roads , houses , tunnels , canals or other ...
A geological basin is a large low-lying area or depression. It is often below sea level. Depressions are typically formed by tectonic processes acting on the lithosphere, providing "accommodation space" for sediment to be preserved. Basins are formed in a variety of tectonic settings: extensional, compressional, strike-slip and intraplate.