Tracking the Seismic Deformation of Himalayan Glaciers Using Synthetic Aperture Radar Interferometry
The Himalayan belt, formed due to the Cenozoic convergence between the Eurasian and Indian craton, acts as a storehouse of large amounts of strain, resulting in large earthquakes from the Western to the Eastern Himalayas. Glaciers also occur over a major portion of the high-altitude Himalayan region...
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| Hauptverfasser: | , , |
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| Format: | Artigo |
| Sprache: | Inglês |
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MDPI AG
2025-03-01
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| Schriftenreihe: | Remote Sensing |
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| Online-Zugang: | https://www.mdpi.com/2072-4292/17/5/911 |
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