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The analysis of the long-period magnetovariation data obtained in the Ukraine and from the project PREPAN-95 are presented. The response functions have been estimated for the harmonics of daily variations for the periods of 4-24 hours using the horizontal spatial gradient method of the magnetic field components. These results together with data of the nearest geomagnetic observatories have given the possibility to compare the mantle geoelectrical structures for three different tectonic regions in the Ukraine. The greatest difference is observed between the Ukrainian shield and the Carpathians together with the Tornquist-Teisseyre zone.
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Rocznik
Tom
Strony
567--573
Opis fizyczny
Bibliogr. 20 poz.
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- Institute of Geophysics, National Academy of Sciences of the Ukraine, Kiev, Ukraine, tectonos@igph.kiev.ua
Bibliografia
Typ dokumentu
Bibliografia
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bwmeta1.element.baztech-article-BSL8-0002-0106