Glacial isostatic uplift of the European Alps
Glacial isostatic uplift of the European Alps
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Publisher
London: Nature Publishing Group UK
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Language
English
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London: Nature Publishing Group UK
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Contents
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 attributed to tectonic shortening, lithospheric delami...
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Full title
Glacial isostatic uplift of the European Alps
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TN_cdi_doaj_primary_oai_doaj_org_article_48d23b8ee0b5409ab1699c18c82c5668
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https://devfeature-collection.sl.nsw.gov.au/record/TN_cdi_doaj_primary_oai_doaj_org_article_48d23b8ee0b5409ab1699c18c82c5668
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ISSN
2041-1723
E-ISSN
2041-1723
DOI
10.1038/ncomms13382
