コメント on "地球最古のオフィオライトの残骸"
Allen P Nutman1, Clark R L Friend
1Institute of Geology, Chinese Academy of Geological Sciences, 26 Baiwanzhuang Road, Beijing 100037, China. nutman@bjshrimp.cn
まとめ
イサウ上皮帯は,主張されているようにオフィオライトの配列を含まないかもしれません. この古代地質学的形成の内部の岩は,異なる年齢のもので,提案されたオフィオライト構成要素の同時代の性質に異議を唱える.
科学分野:
- 地質学 地質学 地質学
- 初期の地球の条件.
- 岩石の形成 岩石の形成 岩石の形成
背景:
- イサウ上皮帯は,約38億年前の地質学的な形成です.
- オフィオライトの配列は,陸上で見つかる海洋の地殻と石層の残骸である.
- 以前の研究では,イシュア上皮帯内のオフィオライト配列の識別が報告されていた.
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