Fault zone damage caused by the mainshock rupture during the 2014 Northern Nagano earthquake
Abstract Seismic velocity variations before and after major earthquakes, measured with ambient noise interferometry, reveal time-dependent changes in subsurface properties, but the physical mechanism that causes them remains difficult to identify. Using noise interferometry, we observed a 0.5–1.3% v...
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| Asıl Yazarlar: | , , |
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| Materyal Türü: | Artigo |
| Dil: | Inglês |
| Baskı/Yayın Bilgisi: |
Nature Portfolio
2025-11-01
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| Seri Bilgileri: | Communications Earth & Environment |
| Online Erişim: | https://doi.org/10.1038/s43247-025-02890-1 |
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