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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 Chedabucto Fault ： ウィキペディア英語版 Chedabucto Fault The Chedabucto Fault is a fault that divides Mainland Nova Scotia from the Minas Basin in the west to Chedabucto Bay in the east into the Avalon zone in the north and the Meguma Zone in the south .The Avalon and Meguma Zones are different because they belonged to different land masses that were widely separated from one another. The Avalon Zone was a part of Laurasia, while the Meguma Zone was a part of Gondwana.It marks the southern margin of the Cobequid Mountains.The Cobequid-Chedabucto Fault Zone is the most prominent geological feature of Nova Scotia. ==References== *(Geology of the Scotian Margin ) *(A synopsis of the geology of the Cobequid Highlands, Nova Scotia ) *(Cobequid-Chedabucto Fault Zone, Nova Scotia ) *(KML reference ) *(Precambrian Period ) 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「Chedabucto Fault」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.