迷路の中の地震:圧縮破裂が2012年のM(w) 8.6のスマトラ地震で分岐した
1Seismological Laboratory, Division of Geological and Planetary Sciences, California Institute of Technology, Pasadena, CA 91125, USA. lsmeng@gps.caltech.edu
まとめ
2012年,スマトラ島で発生した地震.
科学分野:
- 地震学 地震学とは
- 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:
- 2012年のマグニチュード8.6のスマトラ地震は,複雑な破裂ダイナミクスを示した.
- 以前の理解では,ウォートン盆地構造は,ストライク・スリップ・フォールティングによって支配されていたと示唆されていた.
研究 の 目的:
- 2012年スマトラ地震の複雑な破裂プロセスを分析するために.
- ワートン盆地の地震構造を調査する.
主な方法:
- 地震学的観測. 地震学的観測.
- バックプロジェクションソースイメージング.
- ダイナミック・クーロンブ・ストレスの計算.
主要な成果:
- 地震の大きさは,深度,高ストレストドロップ,複数の断層破裂によるものです.
- 断裂は,断裂速度が遅い直交結合断層で発生しました.
- 破裂は東南東西北西の方向に広がり,以前のモデルに挑戦した.
- 破裂は,予測された方向に反して圧縮分岐を示した.
結論:
- 破裂のダイナミクスは,深海の海洋石層の圧力無感強度による制御を示しています.
- オートゴーナル断層と異常な分岐は,ワートン盆地地震構造の理解を広げています.
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