The technology overcomes many limitations of previous airborne EM methods and principles.

The investigation depth range of the system is from near-surface to> 1 km, allowing understanding of shallow and deep geology and mineralization control factors at all scales.

Resistivity resolution is higher and the range of resistivity detection is wider than in the popular time-domain principle.

The high in-depth resolution, depth range, sensitivity to any direction of geoelectrical boundaries, intrinsic to EM methods apparent-conductivity measurement are advantages of the technology.

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