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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 Pan-African orogeny ： ウィキペディア英語版 Pan-African orogeny The Pan-African orogeny was a series of major Neoproterozoic orogenic events (mountain building) which related to the formation of the supercontinents Gondwana and Pannotia about 600 million years ago. This orogeny is also known as the Pan-Gondwanan or Saldanian Orogeny. The Mozambique Belt, extending from east Antarctica through East Africa up to the Arabian-Nubian Shield, formed as a suture between plates during the Pan-African orogeny. The Mozambique ocean began closing between Madagascar-India and the Congo-Tanzania craton between 700 and 580 million years ago, with closure between 600 and 500 million years ago. == References == 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「Pan-African orogeny」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.