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. (e21986). Journal of the Earth and Space Physics, 36(3), e21986
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" .e21986 , Journal of the Earth and Space Physics, 36, 3, 2010, e21986.
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), e21986.
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): e21986,
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. JESP. 2010;36(3):e21986 (In Persian).
