Correction: Corrigendum: Glacial isostatic uplift of the European Alps

Nature Communications 7: Article number:13382 (2016); Published 10 November 2016; Updated 14 July 2017 In an earlier publication, Norton and Hampel proposed post-glacial uplift promoted the re-advance of glaciers at the onset of the Younger Dryas by enlarging their accumulation areas, and estimated...

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Autores principales:	Jürgen Mey, Dirk Scherler, Andrew D. Wickert, David L. Egholm, Magdala Tesauro, Taylor F. Schildgen, Manfred R. Strecker
Formato:	article
Lenguaje:	EN
Publicado:	Nature Portfolio 2017
Materias:	Science Q
Acceso en línea:	https://doaj.org/article/e28567b20e114d50ba0b4c25a21da38f
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spelling	oai:doaj.org-article:e28567b20e114d50ba0b4c25a21da38f2021-12-02T17:06:01ZCorrection: Corrigendum: Glacial isostatic uplift of the European Alps10.1038/ncomms161382041-1723https://doaj.org/article/e28567b20e114d50ba0b4c25a21da38f2017-07-01T00:00:00Zhttps://doi.org/10.1038/ncomms16138https://doaj.org/toc/2041-1723Nature Communications 7: Article number:13382 (2016); Published 10 November 2016; Updated 14 July 2017 In an earlier publication, Norton and Hampel proposed post-glacial uplift promoted the re-advance of glaciers at the onset of the Younger Dryas by enlarging their accumulation areas, and estimated a maximum present-day uplift rate due to deglaciation of ∼0.Jürgen MeyDirk ScherlerAndrew D. WickertDavid L. EgholmMagdala TesauroTaylor F. SchildgenManfred R. StreckerNature PortfolioarticleScienceQENNature Communications, Vol 8, Iss 1, Pp 1-1 (2017)
institution	DOAJ
collection	DOAJ
language	EN
topic	Science Q
spellingShingle	Science Q Jürgen Mey Dirk Scherler Andrew D. Wickert David L. Egholm Magdala Tesauro Taylor F. Schildgen Manfred R. Strecker Correction: Corrigendum: Glacial isostatic uplift of the European Alps
description	Nature Communications 7: Article number:13382 (2016); Published 10 November 2016; Updated 14 July 2017 In an earlier publication, Norton and Hampel proposed post-glacial uplift promoted the re-advance of glaciers at the onset of the Younger Dryas by enlarging their accumulation areas, and estimated a maximum present-day uplift rate due to deglaciation of ∼0.
format	article
author	Jürgen Mey Dirk Scherler Andrew D. Wickert David L. Egholm Magdala Tesauro Taylor F. Schildgen Manfred R. Strecker
author_facet	Jürgen Mey Dirk Scherler Andrew D. Wickert David L. Egholm Magdala Tesauro Taylor F. Schildgen Manfred R. Strecker
author_sort	Jürgen Mey
title	Correction: Corrigendum: Glacial isostatic uplift of the European Alps
title_short	Correction: Corrigendum: Glacial isostatic uplift of the European Alps
title_full	Correction: Corrigendum: Glacial isostatic uplift of the European Alps
title_fullStr	Correction: Corrigendum: Glacial isostatic uplift of the European Alps
title_full_unstemmed	Correction: Corrigendum: Glacial isostatic uplift of the European Alps
title_sort	correction: corrigendum: glacial isostatic uplift of the european alps
publisher	Nature Portfolio
publishDate	2017
url	https://doaj.org/article/e28567b20e114d50ba0b4c25a21da38f
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Correction: Corrigendum: Glacial isostatic uplift of the European Alps

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