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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 Okinawa Trough ： ウィキペディア英語版 Okinawa Trough The (also called (中国語:中琉界沟), literally China-Ryukyu Border Trough ) is a seabed feature of the East China Sea. It is an active, initial back-arc rifting basin which has formed behind the Ryukyu arc-trench system in the West Pacific. It developed where the Philippine Sea Plate is subducting under the Eurasia Plate.〔Thakur, Naresh Kumar ''et al.'' (2010). 〕 ==Description== It is a back-arc basin formed by extension within the continental lithosphere behind the far deeper Ryukyu Trench-arc system.〔Sibuet, Jean-Claude ''et al.'' ("Back arc extension in the Okinawa Trough," ) ''Journal of Geophysical Research,'' Vol. 92, Issue B13, p. 14041-14063.〕 It has a large section more than deep and a maximum depth of . The Okinawa Trough still in an early stage of evolving from arc type to back-arc activity. 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「Okinawa Trough」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.