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Abstract

Based on a large dataset of local body-wave travel times, we determined the first 3-D model of azimuthal P-wave anisotropic tomography of northern Chile in order to study the deformation in the subduction zone. Our results indicate different deformation patterns in the overriding lithosphere, mantle wedge, and the subducting Nazca slab as well as significant along-arc variations. Radiating fast velocity directions (FVDs) around the rupture zone of the 2014 Iquique earthquake (Mw 8.2) are notable in the crust, which may reflect the specific crustal extension induced by a point-like stress source in the form of a fully locked asperity at the plate interface. In most of the study region, FVDs in the mantle wedge are trench-normal, which we interpret to have resulted from mantle wedge flow driven by the oceanic plate subduction. However, trench-parallel FVDs are found beneath the northern segment, which may imply the occurrence of B-type olivine fabrics in the cold forearc mantle. Strong along-arc variations are also observed in the subducting slab, which may reflect intra-slab heterogeneity and change in the slab geometry. In the northern segment, slab bending induces generally trench-normal extension and leads to trench-normal FVDs in the upper part of the slab. In contrast, in the southern segment, flat-slab subduction and thus slab unbending dominates, producing trench-normal compression and trench-parallel FVDs instead. Along the subducting slab interface, FVDs change from trench-parallel to trench normal in the downdip direction, which may indicate the first-order transition from compression in the locking area to dominant shear in the decoupling area along the slab interface.