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. & 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., & 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
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, 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).
