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翻訳と辞書　辞書検索 [ 開発暫定版 ] スポンサード リンク Lenticular bedding ： ウィキペディア英語版 Lenticular bedding Lenticular bedding is a sedimentary bedding pattern displaying alternating layers of mud and sand. Formed during periods of slack water, mud suspended in the water is deposited on top of small formations of sand once the water's velocity has reached zero.〔Terwindt, J. H. J., and Breusers, H. H. C., 1971, Experiments on the Origin of Flaser, Lenticular and Sand-Clay Alternating Bedding(): ''Sedimentology'', v. 19, p. 85-98.〕〔Reineck, H., 1967, Layered Sediments of Tidal Flats, Beaches, and Shelf Bottoms of the North Sea: ''Estuaries'', v. 83, p. 191-206.〕 Lenticular bedding is classified by its large quantities of mud relative to sand, whereas a flaser bed consists mostly of sand. The sand formations within the bedding display a 'lens-like' shape, giving the pattern its respected name. They are commonly found in high-energy environments such as the intertidal and supratidal zones. Geologists use lenticular bedding to show evidence of tidal rhythm, tidal currents and tidal slack, in a particular environment. == References == 〔 抄文引用元・出典: フリー百科事典『 ウィキペディア（Wikipedia）』 ■ウィキペディアで「Lenticular bedding」の詳細全文を読む スポンサード リンク 翻訳と辞書 : 翻訳のためのインターネットリソース Copyright(C) kotoba.ne.jp 1997-2016. All Rights Reserved.