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  • © 2012

Deep Crustal Structure of the Son-Narmada-Tapti Lineament, Central India

  • Nominated for a Springer Theses Prize by the National Geophysical Research Institute, Hyderabad, India
  • The present study provides insight into the subduction/collision history of a seismically significant Central India tectonic zone
  • Comprehensive background information and detailed description of magnetotelluric analyses along four traverses across the Son-Narmada-Tapti Lineament, one of the most prominent geomorphic features in the Indian subcontinent with a length of about 1,200 km
  • Includes supplementary material: sn.pub/extras

Part of the book series: Springer Theses (Springer Theses)

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Table of contents (9 chapters)

  1. Front Matter

    Pages i-xvi
  2. Introduction

    • G. Dhanunjaya Naidu
    Pages 1-11
  3. Magnetotellurics: Basic Theoretical Concepts

    • G. Dhanunjaya Naidu
    Pages 13-35
  4. MT Data Acquisition and Analysis

    • G. Dhanunjaya Naidu
    Pages 37-47
  5. Summary and Conclusions

    • G. Dhanunjaya Naidu
    Pages 139-147

About this book

With a length of about 1200 km, the Son-Narmada-Tapti Lineament (NSL) is one of the most prominent geomorphic features in the Indian subcontinent. Anomalous conductive bodies are delineated at mid-lower crustal depths below major earthquake epicentral zones. The region has been interpreted as the collision zone of the Indian Plate with the Eurasian Plate. The NSL zone is therefore also known to be the second most important tectonic feature in the Indian geology, after the Himalayas.

The present thesis describes significant new insight into the seismotectonics of this Central India tectonic zone, based on thorough magnetotelluric studies. The main objectives of the present study are: (i) to delineate subtrappean sediments across the NSL region along four different traverses, (ii) to understand the characterization of geo-electrical structure of the crust and examine the nature of geo-electrical signatures of the known faults, (iii) to integrate the results with other geophysical data such as seismicity, gravity and heat flow, in order to understand the tectonic scenario of the region.

Deep electromagnetic (magnetotelluric) analyses were integrated in this study with gravity, seismic and heat flow studies and distinct, delineated deep crustal features. The resulting high conductivity is justified with the presence of fluids at mid-lower crustal depths. The migration of these fluids from mantle to mid-lower crustal depths through pre-existing brittle fracture/fault zones were obviously caused by the plume related to the Deccan volcanism. Migration of the fluids generated a higher fluid pressure along the faults and resulted in earthquakes.

Based on the geo-electric sections derived along the four traverses of the Narmada-Son Lineament Zone, the present study gives important clues on the subduction/collision history in this important tectonic zone.

Authors and Affiliations

  • National Geophysical Research Institute, Council of Scientific & Indust. Research, Hyderabad, India

    G. Dhanunjaya Naidu

Bibliographic Information

Buy it now

Buying options

eBook USD 39.99
Price excludes VAT (USA)
  • Available as EPUB and PDF
  • Read on any device
  • Instant download
  • Own it forever
Softcover Book USD 54.99
Price excludes VAT (USA)
  • Compact, lightweight edition
  • Dispatched in 3 to 5 business days
  • Free shipping worldwide - see info
Hardcover Book USD 54.99
Price excludes VAT (USA)
  • Durable hardcover edition
  • Dispatched in 3 to 5 business days
  • Free shipping worldwide - see info

Tax calculation will be finalised at checkout

Other ways to access