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- W2093734577 abstract "Local magnetotelluric sounding data from the Russian Platform are interpreted jointly with global magnetic data of long periodic variations. In the first stage of interpretation the magnetotelluric data are used to find for each site a layered conductivity model for the sediments and the underlying crust and uppermost mantle, regarding the deeper upper mantle as a uniform conductor. In the second stage conductivity estimates are derived down to 1, 200km depth from global data, using for the top layers the results from stage one.The interpretation follows the statistical approach of the NEWTON-LeCAME-MARQUARDT method which takes a random component in the data into account. The best fitting model involves a conductivity increase by two orders of magnitude in 340km depth, even though this result should not be regarded as final and unambiguous." @default.
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- W2093734577 title "Deep Conductivity Distribution on the Russian Platform from the Results of Combined Magnetotelluric and Global Magnetovariational Data Interpretation" @default.
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- W2093734577 doi "https://doi.org/10.5636/jgg.32.supplement1_si105" @default.
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