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tectonic subsidence
Tectonic subsidence is the sinking of the Earth's crust on a large scale, relative to crustal-scale features or the geoid. The movement of crustal plates and accommodation spaces created by faulting create 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.〔Anomalous Cenozoic subsidence along the ‘passive’ continental margin from Ireland to mid-Norway. S. Ceramicola. Science Direct: Marine and Petroleum Geology. 24 November http://www.sciencedirect.com/science/article/pii/S0264817205000723 December 2004〕
== Mechanisms ==
抄文引用元・出典: フリー百科事典『 ウィキペディア（Wikipedia）』
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