Tectonic subsidence is the sinking of the Earth's crust on a large scale, relative to crustal-scale features or the geoid.[1] The movement of crustal plates and accommodation spaces produced by faulting[2] brought about subsidence on a large scale in a variety of environments, including passive margins, aulacogens, fore-arc basins, foreland basins, intercontinental basins and pull-apart basins. Three mechanisms are common in the tectonic environments in which subsidence occurs: extension, cooling and loading.[3][4]
- ^ Makhous, M.; Galushkin, Y. (2005). Basin analysis and modeling of the burial, thermal and maturation histories in sedimentary basins. Editions TECHNIP. p. 66. ISBN 978-2-7108-0846-6. Retrieved 18 November 2011.
- ^ Xie, Xiangyang; Heller, Paul (2006). "Plate tectonics and basin subsidence history". Geological Society of America Bulletin. 121 (1–2): 55–64. doi:10.1130/b26398.1.
- ^ Ceramicola, S.; Stoker, M.; Praeg, D.; Shannon, P.M.; De Santis, L.; Hoult, R.; Hjelstuen, B.O.; Laberg, S.; Mathiesen, A. (2005). "Anomalous Cenozoic subsidence along the 'passive' continental margin from Ireland to mid-Norway". Marine and Petroleum Geology. 22 (9–10): 1045–67. Bibcode:2005MarPG..22.1045C. doi:10.1016/j.marpetgeo.2005.04.005.
- ^ Lee, E.Y., Novotny, J., Wagreich, M. (2019) Subsidence analysis and visualization: for sedimentary basin analysis and modelling, Springer.doi:10.1007/978-3-319-76424-5
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