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Updated: Jul 7, 2026

Data Processing Methods for 3D Seismic Imaging of Subsurface Volcanoes: Applications to the Tarim Flood Basalt
07:58

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非火山による震動と低周波地震は群れをなす

David R Shelly1, Gregory C Beroza, Satoshi Ide

  • 1Department of Geophysics, 397 Panama Mall, Stanford University, Stanford, California 94305-2215, USA. dshelly@pangea.stanford.edu

Nature
|March 16, 2007
PubMed
まとめ

非火山の震動は,断層の近くの地震信号であり,多数の小規模な地震として説明されています. この発見は,震動とスロースリップの出来事が関連した現象であることを示唆し,断層プロセスと地震の危険性についての洞察を提供している.

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