Global demand for metals has risen considerably over the past decade. Geologists are developing new approaches for studying ore deposits and discovering new sources.
Terravox technology allows you to effectively build 2D or 3D models of the high-speed structure of the subsurface space.
The microseismic sounding method offers the opportunity, along with traditional techniques, to verify reliably magnetic anomalies revealing, for example, buried diatremes and determining their spatial parameters, occurrence depth, configuration, sizes, and others features. It is appropriate for assessing volumetric shapes of diatremes and defining their different phases and facies.
Owing to its low cost and high efficiency, this method may be used widely during exploration and study of ore bodies.