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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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Autors principals: Sandeep Kumar Mondal, Rishikesh Bharti, Kristy F. Tiampo
Format: Artigo
Idioma:Inglês
Publicat: MDPI AG 2025-03-01
Col·lecció:Remote Sensing
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Accés en línia:https://www.mdpi.com/2072-4292/17/5/911
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