Fast uplift in the southern Patagonian Andes due to long- and short-term deglaciation and the asthenospheric window underneath
<p>An asthenospheric window underneath much of the South American continent increases the heat flow in the southern Patagonian Andes where glacial–interglacial cycles drive the building and melting of the Patagonian Icefields since the latest Miocene. The Last Glacial Maximum (LGM) was reached...
| Main Authors: | , , |
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| Format: | Article |
| Language: | English |
| Published: |
Copernicus Publications
2024-04-01
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| Series: | Solid Earth |
| Online Access: | https://se.copernicus.org/articles/15/387/2024/se-15-387-2024.pdf |