The conductivity distribution across the Trans-European Suture Zone (TESZ) is presented based on the measurements along a 400 km northeastern directed profile, starting from the German-Polish Basin, crossing the TESZ and ending at the East European Craton. Two-dimensional inversion was applied to magnetotelluric transfer functions and magnetovariational responses corresponding to 38 long-period simultaneously observed sites. Input data for the inversion procedure were created by rotating all transfer functions to strike direction obtained from strike and dimensionality analysis. The results show a thick sedimentary cover, several crustal inhomogeneities and a deep conductive structure below the center of the TESZ. In order to achieve a stable model, several sensitivity analysis were carried out.
Habibian Dehkordi, B. , Oskooi, B. and Brasse, H. (2010). Using the magnetovariational sounding method to image the deep resistivity structure of the Trans-European suture zone. Journal of the Earth and Space Physics, 36(3), -.
MLA
Habibian Dehkordi, B. , , Oskooi, B. , and Brasse, H. . "Using the magnetovariational sounding method to image the deep resistivity structure of the Trans-European suture zone", Journal of the Earth and Space Physics, 36, 3, 2010, -.
HARVARD
Habibian Dehkordi, B., Oskooi, B., Brasse, H. (2010). 'Using the magnetovariational sounding method to image the deep resistivity structure of the Trans-European suture zone', Journal of the Earth and Space Physics, 36(3), pp. -.
CHICAGO
B. Habibian Dehkordi , B. Oskooi and H. Brasse, "Using the magnetovariational sounding method to image the deep resistivity structure of the Trans-European suture zone," Journal of the Earth and Space Physics, 36 3 (2010): -,
VANCOUVER
Habibian Dehkordi, B., Oskooi, B., Brasse, H. Using the magnetovariational sounding method to image the deep resistivity structure of the Trans-European suture zone. Journal of the Earth and Space Physics, 2010; 36(3): -.
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