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Bridging the gap between low-frequency and very-low-frequency earthquakes

Abstract Slow earthquakes that are observed in the > 1 Hz frequency band are called tectonic tremor or low-frequency earthquakes (LFEs) and those in the 0.01–0.10 Hz band are called very-low-frequency earthquakes (VLFEs). These two phenomena are separated by large microseismic noise at 0.1–1.0 Hz. H...

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Principais autores: Koki Masuda, Satoshi Ide, Kazuaki Ohta, Takanori Matsuzawa
Formato: Artigo
Idioma:Inglês
Publicado em: SpringerOpen 2020-04-01
coleção:Earth, Planets and Space
Assuntos:
Low-frequency earthquake
Very-low-frequency earthquake
Broadband slow earthquake
Matched-filter technique
Brownian slow earthquake model
Acesso em linha:http://link.springer.com/article/10.1186/s40623-020-01172-8
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