USING COSMOGENIC 3HE DATING OF ALLUVIAL BOULDERS AS A TOOL FOR CONSTRAINING UPLIFT HISTORY OF THE WESTERN ANDES
The Aroma Quebrada of Northern Chile is a flat lying planation surface underlain by a 16.2 ± 0.7 Ma volcanic deposit (Farías et al. 2005). Boulders collected from the Aroma Quebrada have concentrations of cosmogenic He-3 that require the surface to have been at a low elevation for a substantial period of its history to be consistent with the underlying stratigraphy. This is incompatible with a rapid Late Miocene uplift of the Andes instead the exposure ages restrict the majority of surface uplift of the Western Cordillera to prior to the Late Miocene.
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