Geo Physical Survey

Magnetic Surveys

We measure variations in the Earth's magnetic field to detect underground structures, mineral deposits, and rock types that are magnetic or contain magnetic minerals.

Seismic Surveys

By sending seismic waves through the ground and analyzing their reflections, we map subsurface structures and identify faults, rock layers, and mineral-bearing zones.

Electrical Resistivity Surveys

We use electrical current to measure the resistivity of subsurface materials, helping to locate mineral deposits, groundwater, and other geological features.

Gravity Surveys

By measuring variations in the Earth's gravitational field, we detect density differences in subsurface materials, which can indicate the presence of minerals or oil.

Electromagnetic (EM) Surveys

We use electromagnetic fields to detect conductive minerals such as copper, gold, and nickel, mapping their size, shape, and depth.

Data Processing and Interpretation

Our team of experts processes and interprets all geophysical data using advanced software, providing detailed reports and maps that guide further exploration and development.

Induced Polarization (IP) Surveys

IP surveys are a powerful tool for detecting subsurface minerals such as sulfides, using electrical currents to measure the chargeability of underground materials. We offer various IP survey methods, including:

• Gradient Survey: Ideal for covering large areas quickly, this method provides a broad understanding of chargeability and resistivity over an area.
• Pole-Dipole Survey: This method offers better depth penetration and is particularly useful for mapping deeper mineral bodies
• Dipole-Dipole Survey: Known for its high-resolution data, this method is used to create detailed subsurface images, ideal for identifying smaller or more complex structures.
• Other IP Methods: We can also tailor IP surveys to meet the specific needs of your project, combining various techniques to maximize data quality and exploration success