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Updated: Jul 8, 2026

Blast Quantification Using Hopkinson Pressure Bars
09:41

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Published on: July 5, 2016

大量の一時的な切断ストレスによって引き起こされる非火山性震動.

Justin L Rubinstein1, John E Vidale, Joan Gomberg

  • 1Department of Earth and Space Science, University of Washington, Box 351310, Seattle, Washington, 98195, USA. justin@ess.washington.edu

Nature
|August 3, 2007
PubMed
まとめ

サブダクションゾーン付近の非火山性震動は,遠い地震からの地震波によって引き起こされる可能性があります. これは,振動とスロースリップの出来事が,プレートインターフェースの急速な切断ストレスの増加によって引き起こされることを示唆しています.

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