まとめ
海洋堆積岩は,ベンチュラ盆地が60万年前まで急速に沈んだことを明らかにしています. それ以来,その北端は年間10mm上昇しており,地質学的な速度に匹敵するが,サンアンドレアス断層よりも低い.
科学分野:
- 地質学 地質学 地質学
- 地質物理学 地質物理学とは地質物理学です.
- テクトニクス (地質学) とは
背景:
- ヴェンチュラ盆地の地質史と地質学的な活動は,地域の地殻の動態を理解するために重要である.
- 以前の研究では,長い時間帯における垂直の移動率に関する限られた定量的なデータを提供していた.
研究 の 目的:
- ベンチュラ盆地における過去200万年の縦移の速度を定量化するために.
- 四次元の垂直運動を,最近の地質測定と他の主要な断層系と比較する.
主な方法:
- 海洋堆積岩の分裂軌跡の年代付け.
- 放射線年代測定法 放射線年代測定法
- 年代制限を確立するための古磁気分析.
主要な成果:
- ヴェンチュラ盆地では,約60万年前まで,年間9.5±2.5mmまでの速さで著しい沈没を経験しました.
- 沈下は約060万年前に停止し,その後北流域の限界が上昇した.
- 北の縁は,60万年前から平均10 ± 2mm/年上昇しています.
結論:
- 沈没の停止とそれに続く上昇は,ヴェンチュラ盆地の構造体制の大きな変化を示しています.
- 最近の上昇率は,地質学データと一致しているが,サンアンドレアス断層に沿って観測されたものよりも著しく低い.
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