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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 East African Orogeny ： ウィキペディア英語版 East African Orogeny East African Orogeny is the Neoproterozoic orogeny that affects the East African Orogen.〔Stern, R. J. (1994) Neoproterozoic (900-550 Ma) Arc Assembly and continental collision in the East African Orogen. Annual Review of Earth and Planetary Sciences, 22, 319-351〕 The orogeny evolved from an accretionary orogeny involving the amalgamation of arcs and evolved into a collisional orogeny when the Neoproterozoic continent Azania〔Collins, A.S. and Windley B.F. (2002). The Tectonic Evolution of Central and Northern Madagascar and its place in the Final Assembly of Gondwana. The Journal of Geology, 110: 325-340.〕 collided with the Congo-Tanzania-Bangweulu Block at ~640 Ma.〔Collins, A.S. and Pisarevsky S.A. (2005). Amalgamating eastern Gondwana: The evolution of the Circum-Indian Orogens. Earth Science Reviews. 71: 229-270.〕 The orogeny is the earlier of two orogenies that affects the East African Orogen〔Meert, J.G. (2003). A synopsis of events related to the assembly of eastern Gondwana, Tectonophysics, Volume 362, pp. 1-40.〕 and is followed by the Ediacaran-Cambrian Kuunga Orogeny.〔 == 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「East 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.