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Quaternary landscape evolution of the southern central Andes of Chile quantified using landslide inventories, Be and C1 cosmogenic isotopes and (U-Th)/He thermochronology
(2008-12)
The Andes Mountains--the largest subduction orogen in the world--are a unique natural laboratory suited to test interactions at different timescales between tectonic and surface processes. However, Andean Landscape Evolution ...