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            <funder>G. Aumaître, F. Zaidi and K. Keddadouche are thanked for their valuable assistance during 10Be and 26Al measurements at the ASTER AMS national facility (CEREGE, Aix-en-Provence) which is supported by the INSU/CNRS, IRD and member of Aix-Marseille Platform and REGEF networks. Seismic profiles were interpreted using the MOVE Software Suite donated by PE Limited. We would like to thank the representatives of the IRD in Peru and Ecuador for their support.</funder>
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                <term xml:lang="en">10Be and 26Al cosmogenic isotopes</term>
                <term xml:lang="en">Alluvial fans</term>
                <term xml:lang="en">Active shortening</term>
                <term xml:lang="en">Morpho-tectonic markers</term>
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              <p>Precise dating of geomorphic markers that are subject to thrust-related deformation, such as alluvial fan surface are crucial for quantifying forearc deformation, especially in a context of weak interseismic coupling on the subduction interface as in northern Peru. In this study, we document the late Pleistocene tectonic history of the Amotape massif, which is a prominent basement relief in the northern Peruvian forearc. To achieve this, we combine a morphometric analysis and Terrestrial Cosmogenic Nuclides (TCNs) surface exposure dating of alluvial fan surface with subsurface structural data. TCNs (10Be and 26Al) surface exposure ages of alluvial fan surfaces on the northwestern flank of the massif range from 35.1 ± 1.1 ka to 59.3 ± 2.1 ka for 10Be and from 27.3 ± 2.0 ka to 48.9 ± 2.5 ka for 26Al. Both cosmogenic nuclides provide consistent results. We calculated a mean weighted age of 39.0 ± 0.3 ka for an alluvial fan that is offset by a major NW-verging thrust. Our results provide an estimated slip rate of 1.15 ± 0.46 m/ka along the Amotape thrust front since the late Pleistocene. The surface deformation along the Amotape thrust front correlates with the top portion of a deep-seated contractional wedge involving the crustal basement, according to subsurface structural data and regional seismicity. This integrated analysis demonstrates active shortening in the onshore crustal basement of the northern Peruvian forearc where no active thrust reaching the surface has been described before.</p>
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