Accommodation is a fundamental concept in sequence stratigraphy, a subdiscipline of geology. It is defined as the space that is available for the deposition of sediments.[1][2] Accommodation space can be pictured as the volume between the actual surface and the theoretical equilibrium surface where deposition and erosion are in balance at every point. In marine environments, this equilibrium level is sea level.[3]
In marine environments, changes in accommodation on long temporal scales is mainly determined by tectonics or by changes in eustatic sea level. In fluvial environments, changes in accommodation are controlled by the gradient, discharge and sediment supply. In the lower parts of river systems, the change of accommodation in the fluvial system is controlled by the changes in marine accommodation.[2]
The term is also sometimes used to describe processes by which room is made for plutons to intrude country rock.[4][5]
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References
- ^ Patzkowsky, Mark E.; Holland, Steven M. (2012). Stratigraphic Paleobiology. Chicago: University of Chicago University Press. p. 30.
- ^ a b Catuneanu, Octavian (2011). "Sequence stratigraphy: methodology and nomenclature" (PDF). Newsletters on Stratigraphy. 44 (3). E. Schweizerbart'sche Verlagsbuchhandlung: 173–245. doi:10.1127/0078-0421/2011/0011.
- ^ Boggs, Sam (2006). Principles of sedimentology and stratigraphy (4th ed.). Upper Saddle River, N.J.: Pearson Prentice Hall. p. 451. ISBN 0131547283.
- ^ Fernández, Carlos; Castro, Antonio (August 1999). "Pluton accommodation at high strain rates in the upper continental crust. The example of the Central Extremadura batholith, Spain". Journal of Structural Geology. 21 (8–9): 1143–1149. doi:10.1016/S0191-8141(99)00086-3.
- ^ Acocella, V. (18 January 2002). "Space accommodation by roof lifting during pluton emplacement at Amiata (Italy)". Terra Nova. 12 (4): 149–155. doi:10.1046/j.1365-3121.2000.00286.x. S2CID 128681139. Retrieved 24 July 2020.
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