Foreland basin

（重定向自Foredeep）

Foreland Basin Classes: Peripheral vs. Retroarc

Generalized Foreland Basin System Evolution

A foreland basin is a structural basin that develops adjacent and parallel to a mountain belt. Foreland basins form because the immense mass created by crustal thickening associated with the evolution of a mountain belt causes the lithosphere to bend, by a process known as lithospheric flexure. The width and depth of the foreland basin is determined by the flexural rigidity of the underlying lithosphere, and the characteristics of the mountain belt. The foreland basin receives sediment that is eroded off the adjacent mountain belt, filling with thick sedimentary successions that thin away from the mountain belt. Foreland basins represent an endmember basin type, the other being rift basins. Space for sediments, accommodation space, is provided by loading and downflexure to form foreland basins, in contrast to rift basins, where accommodation space is generated by lithospheric extension.

单词	foredeep
释义	foredeep /fɔ:'di:p/ 英汉-汉英词典 n. 陆外渊；前渊外地槽；深长海沟词组 \| 习惯用语您要查找的是不是： foresee vt. 预知；预见 foretaste n. 预示 forebode v. 预示；预感；预兆 foredoom vt. 注定；预定命运 n. 预定的命运 foredeep n. 陆外渊；前渊外地槽；深长海沟网络短语: foredeep filled 前渊 foredeep basin 前渊盆地 foredeep p 陆外渊 foredeep depression belt 前渊坳陷带 flysch formation in foredeep 前渊复理石英语百科 Foreland basin （重定向自Foredeep） A foreland basin is a structural basin that develops adjacent and parallel to a mountain belt. Foreland basins form because the immense mass created by crustal thickening associated with the evolution of a mountain belt causes the lithosphere to bend, by a process known as lithospheric flexure. The width and depth of the foreland basin is determined by the flexural rigidity of the underlying lithosphere, and the characteristics of the mountain belt. The foreland basin receives sediment that is eroded off the adjacent mountain belt, filling with thick sedimentary successions that thin away from the mountain belt. Foreland basins represent an endmember basin type, the other being rift basins. Space for sediments, accommodation space, is provided by loading and downflexure to form foreland basins, in contrast to rift basins, where accommodation space is generated by lithospheric extension.
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foredeep /fɔ:'di:p/

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网络短语:

Foreland basin