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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 Geology of Antarctica ： ウィキペディア英語版 Geology of Antarctica The geological history of Antarctica covers the geological development of the continent through the Proterozoic Eon, Paleozoic, Mesozoic and Cenozoic eras. More than 170 million years ago, Antarctica was part of the supercontinent Gondwana. Over time Gondwana broke apart and Antarctica as we know it today was formed around 35 million years ago. ==Proterozoic Eon== The Mawson craton of East Antarctica and Australia preserves evidence of tectonic activity from the Archean through the Mesoproterozoic in the Terre Adelie, King George V Land and the Miller Range of the central Transantarctic Mountains.〔Fitzsimmons, I. C. W., ''Proterozoix Basement Provinces of Southern and Southwestern Australia, and There Correlation with Antarctica,'' pp 93-130 in Masaru Yoshida, M., B. F. Windley and S. Dasgupta (eds), ''Proterozoic East Gondwana: Supercontinent Assembly and Breakup,'' Geological Society of London, Special Publication No. 206, 2003 ISBN 978-1862391253〕 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「Geology of Antarctica」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.