Magnetic Survey is an effective and efficient geophysical method that records spatial variations in the Earth’s magnetic field intensity to image anomalies caused by source bodies within the sub-surface, mapping out changes in the amount of magnetic minerals as well as associated rock types. The essential feature is the measurement of the magnetic-field intensity and sometimes the magnetic inclination, or dip, and declination (departure from geographic north) at several stations. 

Our magnetic surveys are valuable for a wide range of applications such as delineating the boundaries of mineral-bearing ore bodies, oil-bearing sedimentary structures, hydrological and environmental searches, cabling and pipelines.