Remote sensing for Earth Science disciplines has proved to be effective in geology. Space and aerial methods allow to measure efficiently and at low-cost the magnetic field - one of the most important indicators in the search for mineral deposits. However, the existing methods have two main shortages: their initial cost is very-high and the global view they provide is impossible to detail. In order to create detailed maps of large territories, there are two options: to decrease the flying height and decrease the flight speed hundreds of times, making it closer to pedestrian pace; or to make sensors work hundreds of times quicker. Existing quantum and proton magnetometers work with limited speed, based on their inherent physical principles. There is only one method left to obtain detailed maps: by ground exploration. It is very expensive and slow, and it sometimes requires huge voltages, especially in the Arctic region, the jungle, the taiga, in mountains and so on. However it is precisely these territories that are the most promising today