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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 Pennine Basin ： ウィキペディア英語版 Pennine Basin The Pennine Basin is a sedimentary basin which was active during the Carboniferous Period and which reached from the Southern Uplands of Scotland in the north to the former Wales-London-Brabant Massif in the English Midlands to the south. Sediments deposited within the basin are now exposed at the surface throughout the Pennines but are also present beneath the surface over a much wider area of northern England and indeed into northeast Wales and just across the border into Scotland.〔Aitkenhead, N. et al 2002 ''British regional geology: the Pennines and adjacent areas'' (4th edn) (British Geological Survey, Nottingham)〕 The basin was complex and consisted, at different times, of a variety of sub-basins separated by blocks across which typically sedimentation continued but resulted in much thinner rock sequences. The term, the 'Pennine Block-and-basin Province' is frequently used in literature to describe the situation which prevailed particularly during the lower Carboniferous. == 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「Pennine Basin」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.