Tracking the Seismic Deformation of Himalayan Glaciers Using Synthetic Aperture Radar Interferometry
Tracking the Seismic Deformation of Himalayan Glaciers Using Synthetic Aperture Radar Interferometry
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Basel: MDPI AG
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English
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Basel: MDPI AG
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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. The impact of earthquakes can be easily studied...
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Full title
Tracking the Seismic Deformation of Himalayan Glaciers Using Synthetic Aperture Radar Interferometry
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TN_cdi_doaj_primary_oai_doaj_org_article_2ea7c62177b948658fc6e3322fc697b8
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https://devfeature-collection.sl.nsw.gov.au/record/TN_cdi_doaj_primary_oai_doaj_org_article_2ea7c62177b948658fc6e3322fc697b8
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ISSN
2072-4292
E-ISSN
2072-4292
DOI
10.3390/rs17050911
