Magnetometry: Proton Precession, Overhauser, Potassium Vapor and Cesium Vapor

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The magnetometry method measures the intensity of the Earth’s total magnetic field, with the purpose of recognizing rock types with different content of magnetic minerals. This method may be done on the ground or with an aircraft, including unmanned aircraft vehicles (UAV). The results have to be later processed and eventually modelled in 3D in order to obtain magnetic susceptibility or amplitude of magnetization distribution.

Instruments

-Six  magnetometers, with improved sensor overhauser 

-Two magnetometers, proton precession

-Two magnetometers, potassium sensor

-Two magnetometers, cesium vapor

-One base station magnetometer, cesium vapor