The Ground Penetrating Geo Complex, known as GPGC "DAUZER", offers a non-intrusive method to investigate the subsurface geological structure at depths ranging from tens to hundreds of meters. DAUZER technology proves highly efficient in geological prospecting and engineering geology.
Incorporating various design and methodological principles, GPGC DAUZER achieves remarkable depths, even in moist clayey soils. It provides valuable information, delineating the boundaries and structures of rock formations.

The high resolution of GPGC imaging allows for detecting minute features in geological structures that traditional geophysical methods cannot reach.
With GPGC data, an experienced geologist can easily identify ore-controlling structures and formations, influencing the determination of confirmatory drilling volumes.

By pinpointing the position and size of these ore-controlling structures, GPGC surveys contribute to confirming the presence of desired mineral deposits, assessing their content and reserves.

This innovative approach has the potential to significantly reduce the need for exploratory and prospecting drilling. GPGC surveys prove effective in exploring various geological structures, including kimberlite pipes, paleochannels, quartz veins, faults, ore bodies, and more.

The Ground Penetrating Geo Complex (GPGC) 'DAUZER' comprises geophysical instruments designed to examine the subsurface structure of soil at variable depths, determined by factors like the instrument model, antenna specifications, and subsurface characteristics.

Its operational principle involves emitting ultra-wideband electromagnetic pulses into the subsurface devoid of a carrier and recording the reflections from layer interfaces or objects.

With its exceptionally powerful pulses, DAUZER excels in functioning within highly conductive environments, such as silt or moist clay. This capability allows it to reach depths of up to 200-300 meters, a feat not achievable by conventional ground-penetrating radar (GPR) equipment.