まとめ
ベネズエラのボコノ断層に沿った氷河期後の移動は,平均66メートルで,年間0.66cmの速度でした. これは,この断層とベネズエラの北海岸に沿って主に重要な構造プレート移動が起こったことを示しています.
科学分野:
- 地質学 地質学 地質学
- テクトニクス (地質学) とは
- 地質物理学 地質物理学とは地質物理学です.
背景:
- ボコノ断層は,ベネズエラの主要な地質構造である.
- 氷河期後の地質学的な動きを理解することは,地震の危険性評価に不可欠です.
研究 の 目的:
- ボコノ断層に沿った氷河後,右側,ストライクスリップの動きを定量化するために.
- 移動の速度とプレートテクトニクスへの影響を決定する.
主な方法:
- 断層の移動を測定するために詳細な地形図の分析.
- 関連する土壌のカーボン14年代測定法により,移動のタイムラインを確立します.
主要な成果:
- ボコノ断層に沿って66メートルの平均的な後氷期右側ストライクスリップ運動.
- 移動速度は年間約0.66センチメートルと推定されています.
結論:
- カリブ海とアメリカ大陸のプレート間の氷河期後の構造プレート移動は,主にボコノ断層とベネズエラの北海岸に沿って発生しました.
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