Geophysical services refer to a branch of geological consulting that provides surveys and reporting to gather, interpret, and map geophysical data. These services are typically used for measuring, analyzing, and optimizing resources for mining or geology, and can also be conducted for engineering, environmental, or other purposes.

MOST COMMON GEOPHYSICAL SURVEYS

There are several different geophysical surveys, all of which use different measurement methods to identify the geography, subsurface artifacts, mineral makeup, etc., of a target area. Knowing which is necessary for your project depends on the stage and scope of your project as well as the geophysical makeup of the territory you are surveying. Below, we discuss the different types of geophysical surveys and what they are used for.

MAGNETIC SURVEY

A magnetic survey is a geophysical survey used to measure and map variations in the Earth’s magnetic field. It uses highly sensitive magnetometers to detect changes in the magnetic properties of subsurface materials and geological features. These variations in magnetic intensity can be caused by different rock types, mineral deposits, or buried structures.

Magnetic surveys are typically used for mineral exploration, archaeology, environmental studies, and oil and gas exploration, as well as to help identify and characterize subsurface features and anomalies.

ELECTROMAGNETIC SURVEYS

Electromagnetic surveys are used to investigate subsurface properties by measuring the response of materials to electromagnetic fields. These surveys involve the transmission of electromagnetic waves into the ground or the surroundings then measuring the signals that are reflected or scattered back. Depending on the method used, electromagnetic surveys can provide information about the electrical conductivity or resistivity of subsurface materials.

This data can be valuable for a wide range of applications, including mineral exploration, groundwater mapping, environmental assessments, and locating buried objects or structures.

ELECTRICAL RESISTIVITY SURVEYS

Electrical resistivity surveys study the subsurface properties of the Earth by measuring the resistance of materials to the flow of electrical currents. In these surveys, electrodes are placed on or in the ground and a small electrical current is passed between them. The resulting voltage measurements are used to calculate the electrical resistivity of the subsurface materials.

Different materials, such as rocks, soils, and groundwater, have varying resistivity values. This means electrical resistivity surveys can provide information about the composition, moisture content, and other geological characteristics of a particular area.

Electrical resistivity surveys are commonly applied in environmental studies, groundwater exploration, engineering projects, and archaeological investigations to map subsurface features, detect anomalies, and assess the suitability of a location for various purposes.

INDUCED POLARIZATION

Induced polarization (IP) surveys investigate subsurface properties by measuring how certain materials respond to electrical currents. In IP surveys, an electrical current is injected into the ground through electrodes, and the voltage decay over time is measured. This type of geophysical survey focuses on the ability of subsurface materials to store and release electrical charge. Materials like minerals or porous rock formations with chargeable properties can exhibit delayed voltage decay, which provides valuable information about their presence and characteristics.

IP surveys are commonly used for mineral exploration, groundwater studies, and environmental investigation. They help geophysicists and researchers identify subsurface anomalies, detect mineral deposits, assess groundwater quality, and evaluate soil and rock properties. 

SEISMIC SURVEYS

Seismic surveys generate seismic waves using controlled sources, then record these waves using geophones or seismometers. In reflection seismic surveys, seismic waves are directed into the ground and bounce back (reflect) off subsurface interfaces (e.g., rock layers or faults). By recording the time it takes for these reflections to return and their amplitudes, geophysicists can create detailed images of the subsurface, revealing the layering and geometry of geological formations.

Refraction seismic surveys measure how seismic waves travel through the subsurface and change direction (refract) when they encounter different geological materials. By analyzing the travel times and angles of refraction, geophysicists can determine subsurface velocities and the depth of geological boundaries.

Seismic surveys help in identifying potential natural resource deposits (like oil, gas, and minerals), evaluating earthquake hazards, assessing groundwater aquifers, and making informed decisions in civil engineering and infrastructure projects. By interpreting seismic data, geoscientists can create subsurface models that aid in resource exploration, environmental studies, and risk assessment.

Final Thoughts

Determining the right geophysical survey for your needs is not only a matter of what will be most effective, but also what is most productive and economical for your project stage. If you’re not sure which geophysical survey is right for your project stage and scope, feel free to reach out and one of our technical service experts will be happy to help.

ABOUT THE AUTHOR

BRIAN GOSS

President, Rangefront Mining Services

Brian Goss brings over 20 years of experience in gold and mineral exploration. He is the founder and President of Rangefront, a premier geological services and mining consulting company that caters to a large spectrum of clients in the mining and minerals exploration industries. Brian is also a director of Lithium Corp. (OTCQB: LTUM), an exploration stage company specializing in energy storage minerals and from 2014 to 2017, he fulfilled the role of President and Director of Graphite Corp. (OTCQB: GRPH), an exploration stage that specialized in the development of graphite properties. Prior to founding Rangefront, Brian worked as a staff geologist for Centerra Gold on the REN project, as well as various exploration and development projects in the Western United States and Michigan. Brian Goss holds a Bachelor of Science Degree with a major in Geology from Wayne State University in Michigan.

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