Brief communication: On the potential of seismic polarity reversal to identify a thin low-velocity layer above a high-velocity layer in ice-rich rock glaciers
<p>Seismic refraction tomography is a commonly used technique to characterise rock glaciers, as the boundary between unfrozen and ice-bearing layers represents a strong impedance contrast. In several rock glaciers, we observed a reversed polarity of the waves refracted by an extended ice-bearing lay...
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| Główni autorzy: | , , , |
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| Format: | Artigo |
| Język: | Inglês |
| Wydane: |
Copernicus Publications
2024-07-01
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| Seria: | The Cryosphere |
| Dostęp online: | https://tc.copernicus.org/articles/18/3231/2024/tc-18-3231-2024.pdf |
| Etykiety: |
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