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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 Giessen nappe ： ウィキペディア英語版 Giessen nappe The Giessen nappe ((ドイツ語:Gießener Decke)) is a tectonic nappe in the southeastern part of the Rhenish Massif in western Germany. The nappe is an "alien" (allochthonous) unit in the Rhenohercynian zone of the Hercynian orogeny, it was thrusted over the usual slightly metamorphosed Devonian and Carboniferous sedimentary rocks in this zone.〔Walter ''et al.'' (1992), p. 179〕 The Giessen nappe is often correlated with the Harz nappe in the Harz〔Huckriede ''et al.'' (2004)〕 and similar units in the Bohemian Massif in the Czech Republic.〔Kalvoda ''et al.'' (2006), pp. 53-54〕 These units form the rare erosional leftovers of small microcontinents that were during the Hercynian orogeny squeezed between the paleocontinents Gondwana to the south and Laurussia to the north. ==Outcrop area== Giessen nappe outcrops cover about 300 km2 from the western edge of the Vogelsberg over Braunfels, Wetzlar and Gießen, almost to Marburg. The river Lahn flows along the northern part of the nappe until it crosses the nappe between Gießen and Wetzlar to continue flowing westwards to the Rhine. 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「Giessen nappe」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.