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...

Celý popis

Uloženo v:
Podrobná bibliografie
Hlavní autoři: Koki Masuda, Satoshi Ide, Kazuaki Ohta, Takanori Matsuzawa
Médium: Artigo
Jazyk:Inglês
Vydáno: SpringerOpen 2020-04-01
Edice:Earth, Planets and Space
Témata:
Low-frequency earthquake
Very-low-frequency earthquake
Broadband slow earthquake
Matched-filter technique
Brownian slow earthquake model
On-line přístup:http://link.springer.com/article/10.1186/s40623-020-01172-8
Tagy: Přidat tag
Žádné tagy, Buďte první, kdo otaguje tento záznam!

Podobné jednotky