Resistivity Imaging From Mt And Seismic Data In The Tucuman Plain, Argentina

MT data along two traverses in the Tucumán Plain<br>were analyzed and it was found that basin sediments<br>are formed mainly by two layers. Then, seismic<br>reflection data coincident to the traverses have been<br>used to constrain the geometry between the basement<br>and the sedimentary rocks. The models obtained<br>from data inversion show a sharp resistivity contrast at the interfaces.