A well-resolved depth to Moho map is presented for the Northern Altiplano.
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A low-velocity zone is identified beneath the active volcanic arc.
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An increase in seismic velocity matches the basal detachment of the Subandean zone.
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Two areas beneath the Eastern Cordillera are thinner than isostatic predictions.
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Our results suggest lower crustal flow and erosion as possible thinning mechanisms.
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