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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 Nordfjord-Sogn Detachment ： ウィキペディア英語版 Nordfjord-Sogn Detachment The Nordfjord—Sogn Detachment (NSD) is a major extensional shear zone up to 6 km in thickness, which extends about 120 km along strike from Nordfjord to Sognefjord, bringing Devonian continental coarse clastic sedimentary rocks into close contact with eclogite facies metamorphic rocks of the Western Gneiss Region. It formed towards the end of the Caledonian Orogeny and was mainly active during the Devonian. It has an estimated displacement of at least 70 km and possible as much as 110 km. It was reactivated during the Mesozoic and may have influenced the development of fault structures in the North Sea rift basin. ==Extent== The NSD is recognised from the western end of the Sognefjord through to the northern shore of Bremanger, a distance of about 120 km. The exposure is fairly continuous, broken occasionally by fjords and some later high-angle faults, such as the Standal Fault. There is evidence from seismic reflection data that the structure continues offshore to the west. 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「Nordfjord-Sogn Detachment」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.