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Glacial isostatic uplift of the European Alps
Following the last glacial maximum (LGM), the demise of continental ice sheets induced crustal rebound in tectonically stable regions of North America and Scandinavia that is still ongoing. Unlike the ice sheets, the Alpine ice cap developed in an orogen where the measured uplift is potentially attr...
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| Veröffentlicht in: | Nat Commun |
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| Hauptverfasser: | , , , , , , |
| Format: | Artigo |
| Sprache: | Inglês |
| Veröffentlicht: |
Nature Publishing Group
2016
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| Schlagworte: | |
| Online Zugang: | https://ncbi.nlm.nih.gov/pmc/articles/PMC5109590/ https://ncbi.nlm.nih.gov/pubmed/27830704 https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1038/ncomms13382 |
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