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This study examines the impact of the March 2015 debris flows in the Atacama Desert on alluvial fan surfaces and channel beds, highlighting the formation of depositional lobes. It proposes a sedimentary and geomorphic sequence to understand landscape modifications and assesses previous interpretations related to paleoclimate reconstructions. The research aims to reconstruct the sedimentary behavior of tributary-junction alluvial fans and their long-term contributions to river systems in the Andes.

Author

albert.cabrecano

Language

EN