دورية أكاديمية
Glacial isostatic uplift of the European Alps.
| العنوان: | Glacial isostatic uplift of the European Alps. |
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| المؤلفون: | Mey J; Institut für Erd- und Umweltwissenschaften, Universität Potsdam, 14476 Potsdam, Germany., Scherler D; Helmholtz Centre Potsdam, GFZ German Research Centre for Geosciences, Telegrafenberg, 14473 Potsdam, Germany.; Institute of Geological Sciences, Freie Universität Berlin, 12249 Berlin, Germany., Wickert AD; Department of Earth Sciences and Saint Anthony Falls Laboratory, University of Minnesota, Minneapolis, 55455 Minnesota, USA., Egholm DL; Department of Geoscience, Aarhus University, 8000 Aarhus, Denmark., Tesauro M; Department of Earth Sciences, Utrecht University, 3508 Utrecht, Netherlands., Schildgen TF; Institut für Erd- und Umweltwissenschaften, Universität Potsdam, 14476 Potsdam, Germany.; Helmholtz Centre Potsdam, GFZ German Research Centre for Geosciences, Telegrafenberg, 14473 Potsdam, Germany., Strecker MR; Institut für Erd- und Umweltwissenschaften, Universität Potsdam, 14476 Potsdam, Germany. |
| المصدر: | Nature communications [Nat Commun] 2016 Nov 10; Vol. 7, pp. 13382. Date of Electronic Publication: 2016 Nov 10. |
| نوع المنشور: | Journal Article; Research Support, Non-U.S. Gov't |
| اللغة: | English |
| بيانات الدورية: | Publisher: Nature Pub. Group Country of Publication: England NLM ID: 101528555 Publication Model: Electronic Cited Medium: Internet ISSN: 2041-1723 (Electronic) Linking ISSN: 20411723 NLM ISO Abbreviation: Nat Commun Subsets: PubMed not MEDLINE |
| أسماء مطبوعة: | Original Publication: [London] : Nature Pub. Group |
| مستخلص: | 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 erosion. Here we show that ∼90% of the geodetically measured rock uplift in the Alps can be explained by the Earth's viscoelastic response to LGM deglaciation. We modelled rock uplift by reconstructing the Alpine ice cap, while accounting for postglacial erosion, sediment deposition and spatial variations in lithospheric rigidity. Clusters of excessive uplift in the Rhône Valley and in the Eastern Alps delineate regions potentially affected by mantle processes, crustal heterogeneity and active tectonics. Our study shows that even small LGM ice caps can dominate present-day rock uplift in tectonically active regions. |
| التعليقات: | Erratum in: Nat Commun. 2017 Jul 14;8:16138. (PMID: 28706286) |
| References: | Nature. 2012 Jul 11;487(7406):219-22. (PMID: 22785319) Sci Rep. 2016 Jun 27;6:28404. (PMID: 27346228) Geomorphology (Amst). 2011 Nov 1;134(1-2):62-78. (PMID: 22053124) Nature. 2010 May 13;465(7295):211-4. (PMID: 20463736) Nat Commun. 2015 Oct 16;6:8605. (PMID: 26472498) Nature. 2013 Oct 31;502(7473):668-71. (PMID: 24172978) |
| تواريخ الأحداث: | Date Created: 20161111 Date Completed: 20180820 Latest Revision: 20181113 |
| رمز التحديث: | 20240628 |
| مُعرف محوري في PubMed: | PMC5109590 |
| DOI: | 10.1038/ncomms13382 |
| PMID: | 27830704 |
| قاعدة البيانات: | MEDLINE |
Full Text Finder | تدمد: | 2041-1723 |
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| DOI: | 10.1038/ncomms13382 |