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Sites glo, pen, and ger are located at the northern segment of the Atacama Fault Zone in the vicinity of the Salar Grande (see Additional files3 and5). These three sites show a similar behavior with respect to phases and apparent resistivities like the exemplary station shown in Figure2. At the surface of this dry, pure halite salar, numerous strike-slip, reverse, normal faults, extensive cracks, and drainage patterns are found (Allmendinger and Gonzales2010; Chong et al.1999) which, if only moderately conductive compared to the salar itself, provide a natural explanation of distortion, together with the observed conductive connection to the Pacific Ocean (see Figure7 (J)). Additionally, conductive near-surface sediments that are younger than the Cordillera basement rocks force current channeling effects. 2b1af7f3a8