Strongly Scattering Medium Along Slow Earthquake Fault Zones Based on New Observations of Short‐Duration Tremors
Résumé
Tremors are a type of slow earthquake with long-duration signals compared to ordinary
earthquakes. The long signals have been considered to solely reflect their long source process. However, here, we provide evidence suggesting that the source processes of tremors are not always long. We refer to these observations as short-duration tremors. They were recorded by ocean-bottom seismometers placed very close to the source. Although these tremors exhibit a short-duration signal when recorded near the source, they exhibit a typical long-duration signal elsewhere. Our numerical simulations demonstrate that the features can be captured by considering a strongly scattering medium around their source. One such structure could be small low-velocity inclusions distributed around the seismic source. The inclusions may represent the seismic expression of geologically detected aquifers in tremor source regions. Furthermore, this medium could be embedded along the slow earthquake fault zone and play a critical role in their source process.
Domaines
Géophysique [physics.geo-ph]
Fichier principal
Geophysical Research Letters - 2023 - Toh - Strongly Scattering Medium Along Slow Earthquake Fault Zones Based on New.pdf (1.78 Mo)
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