地理学 台湾オロゲンにおける層状変形
1Department of Geosciences, National Taiwan University, Taipei, Taiwan.
まとめ
山の形成には 複雑な地殻の動きが伴う 台湾
科学分野:
- 地質学,地質学,構造地質学
背景:
- 収束する縁の山の形成の間に大陸の地殻の押し下ろしは議論の余地があります.
- オロゲン内の変形メカニズムを理解することは,プレート構造の研究にとって極めて重要です.
研究 の 目的:
- 台湾の3次元地震構造を調査する
- 大陸の衝突地帯における 変形過程と地殻層の解明
主な方法:
- 3次元地震性アニソトロピックトモグラフィーを使った.
- 地震波の伝播を分析して 地下組織の方向性や変形を推測した.
主要な成果:
- 台湾の地殻に 2層の変形パターンを観測した
- 上層層は衝突による圧縮変形を示している.
- 下層層は収束に並行するシール変形を示し,これはユーラシアプレートに起因する.
結論:
- 台湾のオロゲンは2層の変形モデルを示しています.
- マントルの石層沈殿によって引き起こされる台湾の山帯の形成には,潜水が重要な役割を果たしています.
- 地震アニソトロピーは,衝突と潜水過程の複雑な相互作用を明らかにします.
関連する概念動画
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