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Fig. 1 | Earth, Planets and Space

Fig. 1

From: Introducing inter-site phase tensors to suppress galvanic distortion in the telluric method

Fig. 1

Plane view of the 3-D synthetic model. The high conductive sedimentary basin (σ=1 S/m and 2 km thick) is shown in gray and the white area represents the surrounding resistive mountains (σ=0.01 S/m). The left side of the vertical fault is coincident with the left side of the basin and the fault is 0 (i.e., no fault) or 2 km wide. The dashed horizontal line depicts the observation profile

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