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| Abstract | We conducted magnetotelluric (MT) field measurements on land and under shallow sea in Horonobe, northern Hokkaido, Japan. We have applied two-dimensional (2D) inversion to land and seafloor MT data simultaneously to obtain seamless resistivity model across the shoreline. In order to deal with both TE- and TM-mode data, static shifts are incorporated as unknowns in the inversion. 2D models by the inversions for two survey lines indicate |
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