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Updated: Jun 23, 2026

Kinematic History of a Salient-recess Junction Explored through a Combined Approach of Field Data and Analog Sandbox Modeling
06:55

Kinematic History of a Salient-recess Junction Explored through a Combined Approach of Field Data and Analog Sandbox Modeling

Published on: August 5, 2016

沈殿板の超低速度層は,メキシコ南部の静かな地震と一致しています

Teh-Ru Alex Song1, Donald V Helmberger, Michael R Brudzinski

  • 1Department of Terrestrial Magnetism, Carnegie Institution of Washington, 5241 Broad Branch Road N.W., Washington, DC 20015, USA. asong@ciw.edu

Science (New York, N.Y.)
|April 25, 2009
PubMed
まとめ

大規模な地震は,閉じられた潜流ゾーンで発生します. メキシコの超低速度層 (USL) は,静かな地震 (スロースリップイベント) と相関し,過渡的な摩擦地帯を明らかにします.

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