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Geo-Electric Crustal Structure Along the Hoshangabad-Ner (HN) Traverse Across the NSL Zone

  • G. Dhanunjaya Naidu
Chapter
Part of the Springer Theses book series (Springer Theses)

Abstract

Another N–S trending traverse of about 270 km length has been covered across the NSL zone. This traverse (Fig. 6.1) lies between the latitudes 20° and 23° close to the longitude of 77.5° and crosses all the major lineaments, faults and different surface geological features.

Keywords

Apparent Resistivity Deccan Trap Induction Vector Impedance Tensor Shallow Section 
These keywords were added by machine and not by the authors. This process is experimental and the keywords may be updated as the learning algorithm improves.

References

  1. 1.
    Kaila KL, Reddy PR, Dixit MM, Koteswara Rao P (1985) Crustal structure across Narmada–Son lineament, Central India from deep seismic soundings. J Geol Soc India 26:465–480Google Scholar
  2. 2.
    Verma RK, Benarjee P (1992) Nature of continental crust along the Narmada–Son lineament, inferred gravity and deep seismic sounding data. Tectonophysics 202:375–397CrossRefGoogle Scholar

Copyright information

© Springer-Verlag Berlin Heidelberg 2012

Authors and Affiliations

  1. 1.MagnetotelluricsCSIR–National Geophysical Research InstituteHyderabadIndia

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