まとめ
インド洋中部の低カリウムトレイイチス基岩は,大西洋と太平洋の標本と一致する. 近くの海底山は,異なるトレイイート基岩を産出し,おそらく最近の低気圧を示している.
科学分野:
- 海洋地質学と地球化学
- 海洋の火山活動について
背景:
- インド洋中部の山脊の火山活動
- 海洋玄武岩の構成は,海洋玄武岩の構成である.
研究 の 目的:
- 中部インド洋のと近くの海底山からの玄武岩を特徴付けます.
- 発見を世界の海洋玄武岩データと比較する.
主な方法:
- 岩石のサンプルを採取するためのドレージ・ハール.
- バサルトの化学および鉱物学的分析
主要な成果:
- インド洋中部の山脊で見つかった低カリウムトレイイチス基岩は,大西洋と太平洋の基岩に似ています.
- 近くの海底山から採取したトーレイト基岩は,より高いKとTi,より低いSiとCaを示しています.
- 一つのサンプルにおける膀の質感は,置換後のうつ状態を示唆している.
結論:
- インド洋中部ののベースルト岩は,化学的に他の主要な海洋盆地で見つかった岩と似ています.
- インドネシア溝の近くの玄武岩における地質化学的変動は,局所的な構造学的な活動を示す可能性がある.
- スピリタイゼーションの証拠は観察されず,置換後の変化が限られていることを示唆しています.
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