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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Detalles Bibliográficos
Autores principales: Mey, Jürgen, Scherler, Dirk, Wickert, Andrew D., Egholm, David L., Tesauro, Magdala, Schildgen, Taylor F., Strecker, Manfred R.
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Nature Publishing Group 2016
Materias:
Article
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC5109590/
https://www.ncbi.nlm.nih.gov/pubmed/27830704
http://dx.doi.org/10.1038/ncomms13382

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC5109590/
https://www.ncbi.nlm.nih.gov/pubmed/27830704
http://dx.doi.org/10.1038/ncomms13382

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