Hight-by-Hight Structure of Magnetic Anomalies Based on Gradient Measurements in the Stratosphere

摘要

A technique has been proposed for recalculating the anomalous magnetic field at altitudes of 20-40 km. Experimental data on induction of the anomalous magnetic field and its vertical gradient, as well as on the vertical gradient increments obtained from balloon gradient magnetic measurements in the stratosphere, are used in the technique. The hight-by-hight structure of the Transbaikalian magnetic anomalies, which made it possible to estimate the specific features of the proposed method of field recalculation, has been constructed. The use of the obtained hight-by-hight structure of the magnetic anomalies in solving certain geophysical problems is illustrated.