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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 Carpathian Flysch Belt ： ウィキペディア英語版 Carpathian Flysch Belt The Carpathian Flysch Belt is an arcuate tectonic zone included in the megastructural elevation of the Carpathians on the external periphery of the mountain chain. Geomorphologically it is a portion of Outer Carpathians. Geologically it is a thin-skinned thrust belt, formed by rootles nappes consisting of so-called flysch - alternating marine deposits of claystones, shales and sandstones which were detached from their substratum and moved tens of kilometers to the north (generally). The Flysch Belt is together with Neogene volcanic complexes only tectonic zone occurring along the whole Carpathian arc. == Areal extent == The Carpathian Flysch Belt is connected to the flysch belt of the Alps (Rhenodanubian Flysch) and continues through the territory of Bohemia, Slovakia, Poland, Ukraine and Romania. Belt is about 1,300 km long and 60 – 75 km wide.〔Veľký, J. (Ed.), 1978, ''Encyclopaedia of Slovakia vol. II. E - J.'' Veda, Bratislava, pp. 103 (In Slovak)〕 Sequences of the Flysch belt are thrusted over the margin of Carpathian foredeep in the north. Foreland of the Flysch belt is build by Bohemian Massif in the west, East-European Platform in the north and Moesian Platform in the east. In the south it is bounded by the Pieniny Klippen Belt in its western segment. Southern boundary of the Flysch Belt in the area of Romanian Carpathians covered by nappes of the crystalline-Mesozoic zone.〔Dumitrescu, I., Sandulescu, M., 1974, Flysch Zone. in Maheľ, M. (Ed.) ''Tectonic of the Carpathian Balkan Regions.'' Carpathian-Balkan Association – Commission for Tectonics. Geological Institute of Dionýz Štúr, Bratislava, pp. 253-264〕 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「Carpathian Flysch Belt」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.