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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 Portsdown Anticline ： ウィキペディア英語版 Portsdown Anticline The Portsdown Anticline is a north-facing geological fold of Tertiary age affecting rocks in Hampshire, southern England.〔Toghill, P. 2000 ''The Geology of Britain: an introduction'' Crowood Press, Marlborough Wilts p166〕 This upfold of the local sedimentary rock sequence is paralleled by the Bere Forest/Chichester Syncline (downfold) about 2km to its north and a postulated deep fault to the north again. Further west, this major east-west structure adopts more of a NW - SE alignment.〔Melville, R.V. and Freshney, E.C. 1982 ''British Regional Geology: The Hampshire Basin and adjoining areas'' IGS/NERC, London p116 & 121〕 At the surface the Portsdown Anticline is seen to affect the Chalk rocks of Late Cretaceous age at Ports Down though it is known to also affect the underlying Jurassic strata.〔British Geological Survey 1998 ''Fareham'' England and Wales sheet 316 Solid and drift geology. 1:50,000 (Keyworth, Nottingham: BGS)〕 == 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「Portsdown Anticline」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.