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Updated: Jun 26, 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

プレート界面の近くに位置するカスカディア震動は,S マイナス P 波の倍数によって制約されます

Mario La Rocca1, Kenneth C Creager, Danilo Galluzzo

  • 1Istituto Nazionale di Geofisica e Vulcanologia-Osservatorio Vesuviano, Via Diocleziano 328, 80124 Napoli, Italy. mlarocca@ov.ingv.it

Science (New York, N.Y.)
|January 31, 2009
PubMed
まとめ

非火山の振動を特定することは難しい. この研究では,地震波 (S波とP波) のタイムラグを使用して,震動源の深さを正確に特定し,その震動源が潜水板の近くから発生していることを明らかにします.

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