Tectonic Tremor Explained by Successive Ruptures of Clustered Quartz‐Filled Shear Veins
Abstract A tectonic tremor is a successive seismic signal observed along plate boundaries in subduction zones. However, the source processes and mechanisms responsible for the tremor remain unclear. Quartz‐filled shear and extension veins are clustered in tens to hundreds of meters thick subduction...
Tallennettuna:
| Päätekijät: | , |
|---|---|
| Aineistotyyppi: | Artigo |
| Kieli: | Inglês |
| Julkaistu: |
Wiley
2025-07-01
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| Sarja: | Geophysical Research Letters |
| Aiheet: | |
| Linkit: | https://doi.org/10.1029/2025GL115447 |
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