Application of Altitude Models of Earth’s Magnetic Field for Solving Geophysical Problems


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Abstract

The role of altitude models of Earth’s magnetic field for solving geophysical problems using spacecraft is considered. The results of studying the features of the deep structure of Earth’s crust in the structure of magnetic anomalies according to the data of satellite altitude measurements on the CHAMP mission are presented. The informativity of the components of the magnetic anomalies in near-Earth space calculated by the component model of Earth’s magnetic field is presented for searching for minerals in the geothermal regions of Central Europe and North America, in the zone of deposits of ferruginous quartzites of the Baltic shield, and hydrocarbon deposits in the oil and gas basins of Tatarstan, Siberia, the Barents, Mediterranean, and North seas.

About the authors

Yu. A. Kopytenko

Pushkov Institute of Terrestrial Magnetism, Ionosphere, and Radio Wave Propagation, St. Petersburg Branch,
Russian Academy of Sciences

Email: p.v.labetskiy@gmail.com
Russian Federation, St. Petersburg, 199034

A. A. Petrova

Pushkov Institute of Terrestrial Magnetism, Ionosphere, and Radio Wave Propagation, St. Petersburg Branch,
Russian Academy of Sciences

Email: p.v.labetskiy@gmail.com
Russian Federation, St. Petersburg, 199034

V. F. Alekseev

Mozhaysky Military Space Academy

Email: p.v.labetskiy@gmail.com
Russian Federation, St. Petersburg, 197082

I. S. Gur’ev

Mozhaysky Military Space Academy

Email: p.v.labetskiy@gmail.com
Russian Federation, St. Petersburg, 197082

P. V. Labetskiy

Mozhaysky Military Space Academy

Author for correspondence.
Email: p.v.labetskiy@gmail.com
Russian Federation, St. Petersburg, 197082

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