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MTS studies were carried out using the Promega CellTiter 96 AQueous One Solution Cell Proliferation Assay (Promega, Madison, WI, USA).
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MT studies reveal that the observed electric field is always affected by the distortion effect.
We believe that this type of survey represents an attractive complement to traditional marine MT studies based on sea-bottom vector measurements.
However, earlier MT studies also observed similar conducting features in the lower crust in the Son Narmada Region extending north of Narmada River (Gokarn et al., 2001).
Similar integration of Faraday's law has been previously used by Becken and Pedersen (2003) and Becken et al. (2008) in MT studies.
There have been few MT studies carried out in central India over the Deccan volcanic province across the major fault zones.
Earlier MT studies suggest that lower-crustal zones exhibit relatively conductive environments with respect to seismogenic brittle crust (Jiracek et al. 2007).
MT studies aimed at investigating the relationship between the fault and the electrical resistivity structure have been carried out in many major fault regions around the world.
The inducing geomagnetic field variation B is assumed to be located far from the observation site and to be a plane wave in MT studies.
This is often assumed as the normal mode in MT studies, so that the anomalous fields are created by additional 2D or 3D conductivity structures.
Moreover, as is usual practice in MT studies, their method works in the frequency/wavenumber domain and assumes quasi-uniform sources.
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