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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 Barents Basin ： ウィキペディア英語版 Barents Basin The Barents Basin or East Barents Basin is a sedimentary basin underlying the eastern half of the Barents Sea. Lying off Russia on the continental shelf between the Kola Peninsula and Novaya Zemlya, it produces oil and gas.〔Funk, McKenzie (May 2009) "Arctic Landgrab" ''National Geographic'' 215(5): pp. 104–121〕 The Barents Basin is bordered by land and the Timan-Pechora Basin to the south, the Murmansk Rise and Murmansk Plateau to the west, the Admiralty High and the island of Novaya Zemlya to the east, and rise of Franz Josef Land to the north. The Barents Basin is subdivided into the South Barents Basin (south of the Ludlov Saddle), the North Barents Basin, and the North Novaya Zemlya Basin. The latter two are separated by a major NW–SE fault.〔Doré, A. G. (1995) "Barents Sea Geology, Petroleum Resources and Commercial Potential" ''Arctic'' 48(3): pp. 207–221〕 ==Geology== Beginning in the late Palaeozoic and continuing through to the early Cretaceous sediments were deposited on the continental shelf of the supercontinent Pangaea, these underlie the current Barents Basin which was created during the break-up of Pangaea. Beginning in the Cretaceous a rift zone opened between the Baltic Plate and the Siberian Plate, parallel to and west of the old Ural Mountains suture zone, represented here by Novaya Zemlya.〔 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「Barents 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.