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

Naidu, G. Dhanunjaya Dhanunjaya

9783662521816: Deep Crustal Structure of the Son-Narmada-Tapti Lineament, Central India

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ISBN 10 : 3662521814 ISBN 13 : 9783662521816

Editeur : Springer, 2016

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This book reviews new insights into the seismotectonics of this Central India tectonic zone, based on magnetotelluric studies. Integrates deep electromagnetic analyses with gravity, seismic and heat flow studies and distinct, delineated deep crustal features.

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�diteur: Springer
Date d'�dition: 2016
Langue: anglais
ISBN 10: 3662521814
ISBN 13: 9783662521816
Reliure: Broch�
Nombre de pages: 164
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9783642284410: Deep Crustal Structure of the Son-Narmada-Tapti Lineament, Central India: Doctoral Thesis Accepted Byh the Osmania University, Hyderabad, India

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ISBN 10 : 3642284418 ISBN 13 : 9783642284410
Editeur : Springer-Verlag Berlin and Heide..., 2012
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Deep Crustal Structure of the Son-Narmada-Tapti Lineament, Central India

G. Dhanunjaya Naidu

Edit� par Springer Berlin Heidelberg, 2016

ISBN 10 : 3662521814 ISBN 13 : 9783662521816

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Deep Crustal Structure of the Son-Narmada-Tapti Lineament, Central India (Springer Theses)

Naidu, G. Dhanunjaya

Edit� par Springer, 2016

ISBN 10 : 3662521814 ISBN 13 : 9783662521816

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

G. Dhanunjaya Naidu

Edit� par Springer Berlin Heidelberg, 2016

ISBN 10 : 3662521814 ISBN 13 : 9783662521816

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Taschenbuch. Etat : Neu. Druck auf Anfrage Neuware - Printed after ordering - 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. N� de r�f. du vendeur 9783662521816

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

G. Dhanunjaya Naidu

Edit� par Springer Berlin Heidelberg Aug 2016, 2016

ISBN 10 : 3662521814 ISBN 13 : 9783662521816

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Vendeur : BuchWeltWeit Ludwig Meier e.K., Bergisch Gladbach, Allemagne

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Taschenbuch. Etat : Neu. This item is printed on demand - it takes 3-4 days longer - Neuware -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. 164 pp. Englisch. N� de r�f. du vendeur 9783662521816

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

G. Dhanunjaya Naidu

Edit� par Springer, Springer Berlin Heidelberg Aug 2016, 2016

ISBN 10 : 3662521814 ISBN 13 : 9783662521816

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Vendeur : buchversandmimpf2000, Emtmannsberg, BAYE, Allemagne

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Taschenbuch. Etat : Neu. This item is printed on demand - Print on Demand Titel. Neuware -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.Springer-Verlag GmbH, Tiergartenstr. 17, 69121 Heidelberg 164 pp. Englisch. N� de r�f. du vendeur 9783662521816

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