Conventional ERT is widely used in mineral exploration, but often runs up against limitations in the field or fails to investigate deeper structures.

Our advanced approach delivers 3D resistivity and IP models down to 1.5 kilometers, supported by a flexible acquisition network that adapts seamlessly to any topography or inhabited area. Deep Electrical Resistivity Tomography is an ideal tool for geothermal exploration. It allows us to directly image conductive regions enriched in fluids, such as aquifers, which can be harnessed for heat production.

If your project targets a specific fault system that channels hot fluids or can be engineered in this way, we can detect it by identifying lithological contrasts created by the fault itself or by pinpointing zones where the fault facilitates the circulation of fluids through the crust.  We adapt our survey to all scales, from the development of geothermal power plants to the research of water or heat sources for private customers.