Glacial isostatic uplift of the European Alps
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منابع مشابه
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 attributed to tectonic shortening, lithospheric delamination and unloading due to deglaciation and er...
متن کاملCorrigendum: Glacial isostatic uplift of the European Alps
This corrects the article DOI: 10.1038/ncomms13382.
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ژورنال
عنوان ژورنال: Nature Communications
سال: 2016
ISSN: 2041-1723
DOI: 10.1038/ncomms13382