Glacial-isostatic-adjustment strain rate–stress paradox in the Western Alps and impact on active faults and seismicity
<p>In many regions formerly glaciated during the Last Glacial Maximum (LGM), glacial isostatic adjustment (GIA) explains most of the measured uplift and deformation rates. GIA is also proposed as a key process contributing to fault activity and seismicity shortly after the LGM and potentially...
| Main Authors: | , , |
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| Format: | Article |
| Language: | English |
| Published: |
Copernicus Publications
2023-10-01
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| Series: | Solid Earth |
| Online Access: | https://se.copernicus.org/articles/14/1067/2023/se-14-1067-2023.pdf |