• Gundumalla Mahesh
• Veeraiah, B.
• Devaiah Narmala

The magnetic method is based on the measurement of earth's induced magnetic field and through the detection of magnetic anomalies that are generally caused by subsurface susceptibility contrasts. Generally the magnetic susceptibility varies significantly between different rock types. Sedimentary rocks have the lowest average susceptibility and the basic igneous the largest. The end product of a magnetic survey (land, sea or airborne) is a set of profiles or a contour map of magnetic features of subsurface targets and structures. Modeling of magnetic anomalies is similar in procedure to that in gravity as both these techniques utilize natural potential fields.

Geophysics, Total Magnetic Intensity, Reduction to Pole, exploration, ground magnetic survey, GSM-19 WALKMAG magnetometers.

"GROUND MAGNETIC STUDIES FOR IRON ORE EXPLORATION IN NORTHERN PART OF THE MAYURBHANJ DISTRICT, ODISHA, INDIA.", International Journal of Emerging Technologies and Innovative Research (www.jetir.org), ISSN:2349-5162, Vol.9, Issue 5, page no.j157-j163, May-2022, Available :http://www.jetir.org/papers/JETIR2205A25.pdf

"GROUND MAGNETIC STUDIES FOR IRON ORE EXPLORATION IN NORTHERN PART OF THE MAYURBHANJ DISTRICT, ODISHA, INDIA.", International Journal of Emerging Technologies and Innovative Research (www.jetir.org | UGC and issn Approved), ISSN:2349-5162, Vol.9, Issue 5, page no. ppj157-j163, May-2022, Available at : http://www.jetir.org/papers/JETIR2205A25.pdf