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Electrical signatures of the Earth’s crust in central India as inferred from magnetotelluric study

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Figure

Fig. 1. Location of the Hoshangabad-Ner traverse (MT soundings are black triangles) plotted on a geological and tectonic map of the present study area(GSI, 2000)
Fig. 2. (a) A typical example of MT data for station 12. (b) Best fitted regional strike direction of N70◦E and its 90◦ ambiguity N20◦W are plottedusing the Groom-Bailey decomposition technique (Rose diagram) in the frequency range of 100–0.001 Hz considering all the stations.
Fig. 3. (a) Dimensionality parameters (Swift’s and Bahr’s skew) are plotted for the present data set
Fig. 4. The Bouguer gravity anomaly (a) plotted over the deep geoelectric crustal section (b)
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