アメリカ合衆国北東部の地殻構造:グレンビル州とアパラチア州との対比
まとめ
地殻モデルは,米国北東部の独特の地質構造を明らかにしています. ニューイングランド・アパラチア山脈は,2層の地殻を示しており,同質なプレキャンブリア・グレンヴィル州とは異なっており,多種多様な構造進化を示唆している.
科学分野:
- 地質物理学 地質物理学とは地質物理学です.
- 地震学 地震学とは
- テクトニクス (地質学) とは
背景:
- 地域地殻の構造を理解することは,構造的進化の解釈に極めて重要です.
- 米国北東部の地殻に関する以前のモデルは,詳細な解像度が欠けていました.
研究 の 目的:
- 米国北東部の平均地殻モデルを計算する.
- 異なる地質省間の地殻構造の変動を調査する.
主な方法:
- 地域地震によるP波とS波の移動時間の分析.
- P(n) の地震波データを用いて時間分析の適用.
主要な成果:
- プレカンブリア時代のグレンヴィル州は,均質な地殻を示しています.
- パレオゾイク新イングランド・アパラチア山脈は,2層の地殻と高速下層を呈している.
- 厚いか低速の地殻が,地質構造に並行して,ニューイングランド中部で確認された.
結論:
- 異なる地殻構造は,異なる地質学的な地域 (グレンビルとニューイングランド・アパラチア) と相関しています.
- 観測された地殻の差異は,2つの地域の対照的な構造の歴史から生じる可能性が高い.
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