Along strike variations on inverted Tarapaca Basin and its influence in buried western Andean mountain front building

Recent studies focus in the forearc tectonic and structural evolution evidencing the strong control of the preorogenic structures in the accommodation of the Andean shortening and deformation. Lateral variations in the structures of mountain fronts can generate relevant changes in the crustal shortening magnitudes and lead to variations in tectonic models. The Western Andean Mountain Front at 21 degrees S represents a unique opportunity to understand the interplay between inherited extensional fabric and thrust belt front structures related to orogenic processes. To assess the structural style, along strike variations and tectonic evolution, we combined regional field observations, 2D seismic interpretation calibrated by well data and rock outcrops, balanced structural crosssections, aero-magnetic data, structural interpretation and 3D structural modelling. The main results validated and latitudinally extended the structural style characterized by partially inverted graben and half-graben arrays formed by Jurassic to Early Cretaceous extension and subsequently underwent contraction which led to the basin inversion at least since the Upper Cretaceous. This contribution also shows for the first time a complete 3D structural framework showing lateral continuation of main structures and the relationship between orogenparallel (N-S and NNE-SSW trends) and orogen-oblique structures (ENE-WSW, NW-SE and WNW-ESE orientations), being plausible to propose tip points, polarity changes and accommodation zones. Partially inverted graben and half-graben arrays, accommodation zones, its evolution and along strike variations must be consider in tectonic and generative exploration models to better understand the main Andean structures and mineral deposits distribution, respectively.