Fast uplift in the southern Patagonian Andes due to long- and short-term deglaciation and the asthenospheric window underneath

Fast uplift in the southern Patagonian Andes due to long- and short-term deglaciation and the asthenospheric window underneath

<p>An asthenospheric window underneath much of the South American continent increases the heat flow in the southern Patagonian Andes where glacial–interglacial cycles drive the building and melting of the Patagonian Icefields since the latest Miocene. The Last Glacial Maximum (LGM) was reached...

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Bibliographic Details
Main Authors: V. A. P. Muller, P. Sternai, C. Sue
Format: Article
Language:English
Published: Copernicus Publications 2024-04-01
Series:Solid Earth
Online Access:https://se.copernicus.org/articles/15/387/2024/se-15-387-2024.pdf

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