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The hourly data of nine geomagnetic observatories situated in Central Europe have been analyzed using the generalized magnetovariation (GMV) method designed recently for induction soundings of inhomogeneous media. In this method, impedance is one of transfer functions in the differential relation between spectra of the magnetic components and their derivatives. The peculiarity of this impedance is its correspondence to the magnetotelluric one estimated from the linear relations. Three transfer functions have been estimated simultaneously for data of geomagnetic observatories, using three different routines working in the period range from three hours up to two days. Noises in the source field components have been compared with noise in the estimated plane field divergence. The multivariate errorsin-variables method was used to extract spatially and temporally coherent geomagnetic field structure from the partially incoherent geomagnetic variations. This method allows estimating reliably impedances and gradient tippers for each observatory, taking into consideration the Earth’s sphericity. The obtained responses have been used for induction soundings and for detecting a deep inhomogeneity in the region.
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Tom
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815--832
Opis fizyczny
Bibliogr. 32 poz.
Twórcy
autor
autor
autor
- Institute of Geophysics, Polish Academy of Sciences, Warszawa, Poland, sem@igf.edu.pl
Bibliografia
- Aboul-Atta, O.A., andW.M. Boerner (1975), Vectorial impedance identity for the natural dependence of harmonic fields on closed boundaries, Canadian J. Phys. 53, 15, 1404-1407.
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- Constable, S.C., R.L. Parker, and C.G. Constable (1987), Occam’s inversion: A practical algorithm for generating smooth models from electromagnetic sounding data, Geophysics 52, 289-300.
- Egbert, G.D. (1997), Robust multiple-station magnetotelluric data processing, Geophys. J. Int. 130, 2, 475-496.
- Francis, J.G.F. (1961), The QR transformation a unitary analogue to the LR transformation – Part 1, Comput. J. 4, 3, 265-271.
- Francis, J.G.F. (1962), The QR transformation – Part 2, Computer J. 4, 4, 332-345.
- Fujii, I., and A. Schultz (2002), The 3D electromagnetic response of the Earth to ring current and auroral oval excitation, Geophys. J. Int. 151, 3, 689-709.
- Guglielmi, A.V., and M.B. Gokhberg (1987), On the magnetotelluric sounding in the seismically active areas, Izv. – Phys. Solid Earth 33, 122-123 (in Russian).
- Kharin, E.P., and V.Yu. Semenov (1989), Model of geomagnetic field variations at the period range from 4 days until 3 years, Il Nuovo Cimento 12, 5, 547-554.
- Kuckes, A.F., A.G. Nekut, and B.G. Thompson (1985), A geomagnetic scattering theory for evaluation of Earth structure, Geophys. J. Roy. Astr. Soc. 83, 2, 319-330.
- Kuvshinov, A., H. Utada, D. Avdeev, and T. Koyama (2005), 3-D modelling and analysis of Dst C-responses in the North Pacific Ocean region, revisited, Geophys. J. Int. 160, 2, 505-526.
- Nowozynski, K. (2004), Estimation of magnetotelluric transfer functions in the time domain over a wide frequency band, Geophys. J. Int. 158, 1, 32-41.
- Olsen, N. (1998), The electrical conductivity of the mantle beneath Europe derived from C-responses from 3 to 720 hr, Geophys. J. Int. 133, 2, 298-308.
- Parker, R.L., and K.A. Whaler (1981), Numerical methods for establishing solutions to the inverse problem of electromagnetic induction, J. Geophys. Res. 86, B10, 9574-9584.
- Pushkarev, P.Yu., T. Ernst, J. Jankowski, W. Józwiak, M. Lewandowski, K. Nowozynski, and V.Yu. Semenov (2007), Deep resistivity structure of the Trans-European Suture Zone in central Poland, Geophys. J. Int. 169, 3, 926-940.
- Rytov, S.E. (1940), Calculation of the skin-effect by the perturbation method, J. Exp. Theor. Phys. 10, 2, 180-189 (in Russian).
- Schmucker, U. (1970), Anomalies of Geomagnetic Variations in the Southwestern United States, Univ. California Press, Berkeley, 165 pp.
- Schmucker, U. (2003), Horizontal spatial gradient sounding and geomagnetic depth sounding in the period range of daily variations. In: A. Hördt and J.B. Stoll (eds.), Protokoll über das Kolloquium Elektromagnetische Tiefenforschung, 29.09.-3.10.2003, Königstein, 306-317.
- Schmucker, U. (2008), Comparative induction studies with geomagnetic observatory data in three epochs. In: Abstr. 19th Int. Workshop on Electromagnetic Induction in the Earth, October 23-29, 2008, Beijing, China, 879-884.
- Semenov, V.Yu. (1998), Regional conductivity structures of the Earth’s mantle, Publs. Inst. Geophys. Pol. Acad. Sc. C-65, 302, 122 pp.
- Semenov, V.Yu., and W. Józwiak (2006), Lateral variations of the mid-mantle conductance beneath Europe, Tectonophysics 416, 279-288.
- Semenov, V.Yu., and V.N. Shuman (2010), Impedances for induction soundings of the Earth’s mantle, Acta Geophys. 58, 4, 527-542.
- Semenov, V.Yu., J. Pek, A. Ádám, W. Józwiak, B. Ladanyvskyy, I.M. Logvinov, P. Pushkarev, J. Vozár, and Experimental Team of CEMES Project (2008), Electrical structure of the upper mantle beneath Central Europe: Results of the CEMES Project, Acta Geophys. 56, 4, 957-981.
- Senior, T.B.A., and J.L. Volakis (1995), Approximate boundary conditions in electromagnetics, IEE Press, London, 353 pp.
- Shuman, V.N. (1999), Scalar local impedance conditions and the impedance tensor in processing and interpretation of a magnetotelluric experiment, Geophys. J. Kiev 19, 361-385.
- Shuman, V. (2007), Imaginary surface vectors in multidimensional inverse problems of geoelectrics, Izv. – Phys. Solid Earth 43, 3, 205-210.
- Shuman, V., and S. Kulik (2002), The fundamental relations of impedance type in general theories of the electromagnetic induction studies, Acta Geophys. Pol. 50, 4, 607-618.
- Vanyan, L.L., V.A. Kuznetsov, T.V. Lyubetskaya, N.A. Palshin, T. Korja, I. Lahti, and BEAR Working Group (2002), Electrical conductivity of the crust beneath Central Lapland, Izv. – Phys. Solid Earth 38, 10, 798-815.
- Vozár, J., and V.Yu. Semenov (2010), Compatibility of induction methods for mantle soundings, J. Geophys. Res. 115, B03101.
- Vozár, J., V.Y. Semenov, A.V. Kuvshinov, and C. Manoj (2006), Updating the map of Earth’s surface conductance, Eos Trans. AGU 87, 33, 326.
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Bibliografia
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bwmeta1.element.baztech-article-BSL1-0015-0012