 The research explores the Benitos-Galit geothermal field using an audio-magnetoluric survey to understand the link between the geothermal fluid path and main geological structures, suggesting a deep-rooted NS fault system controls the flow path. A conductive heat-driven system is proposed, taking into consideration the geologic setting and low geothermal gradient of this tectonic environment. Further investigations are needed to assess the geothermal potential of the study area. This article was authored by H. Barcelona, G. Perry, D. Winniker, and others.