Long-term dynamic topographic support during post-orogenic crustal thinning revealed by stable isoto...
Long-term dynamic topographic support during post-orogenic crustal thinning revealed by stable isotope (δ18O) paleo-altimetry in eastern Pyrenees
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London: Nature Publishing Group UK
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English
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London: Nature Publishing Group UK
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Understanding the geodynamic and Earth surface processes at the origin of post-collisional surface uplift in mountain ranges requires reconstruction of paleo-elevation. Here, we focus on the topographic evolution of the Cerdanya Basin in the eastern Pyrenees formed by post-orogenic extension during the Late Miocene. Stable isotope (δ
18
O) an...
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Long-term dynamic topographic support during post-orogenic crustal thinning revealed by stable isotope (δ18O) paleo-altimetry in eastern Pyrenees
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TN_cdi_pubmedcentral_primary_oai_pubmedcentral_nih_gov_7010729
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https://devfeature-collection.sl.nsw.gov.au/record/TN_cdi_pubmedcentral_primary_oai_pubmedcentral_nih_gov_7010729
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ISSN
2045-2322
E-ISSN
2045-2322
DOI
10.1038/s41598-020-58903-w