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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 Vegetation-induced sedimentary structures ： ウィキペディア英語版 Vegetation-induced sedimentary structures Vegetation-induced sedimentary structures (VISS) are primary sedimentary structures formed by the interaction of detrital sediment with ''in situ'' plants. VISS provide physical evidence of vegetation's fundamental role in mediating sediment accumulation and erosion in clastic depositional environments.〔Rygel, M.C., Gibling, B.C. and Calder, J.H. (2004) Vegetation-induced sedimentary structures from fossil forests in the Pennsylvanian, Joggins Formation, Nova Scotia; Sedimentology, v. 51,p. 531-552.〕 VISS can be broken into seven types, five being hydrodynamic and two being decay-related. The simple hydrodynamic VISS are categorized by centroclinal cross strata, scratch semicircles and upturned beds. The complex hydrodynamic VISS are categorized by coalesced scour fills and scour-and-mound beds. The decay-related VISS are categorized by mudstone-filled hollows and downturned beds.〔 == Hydrodynamic structures == 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「Vegetation-induced sedimentary structures」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.