Abstract:<p>Constraining the impact of Quaternary glaciations on landscape dynamics is required to better understand the interaction between tectonics, climate, and erosion. Over the years, low-temperature thermochronology such as apatite (U-Th)/He (AHe) has been used to quantify glacial erosion in different climatic and tectonic settings. However, in some contexts, AHe records lack temporal resolution because of limited exhumation due to glacial incision and/or low geothermal gradients. In addition, sign… Show more
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