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Deep Crustal Structure of the Son-Narmada-Tapti Lineament, Central India: Doctoral Thesis Accepted Byh the Osmania University, Hyderabad, India - Couverture rigide
Synopsis
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.Les informations fournies dans la section « Synopsis » peuvent faire référence à une autre édition de ce titre.
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Deep Crustal Structure of the Son-Narmada-Tapti Lineament, Central India : Doctoral Thesis Accepted Byh the Osmania University, Hyderabad, India
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Deep Crustal Structure of the Son-Narmada-Tapti Lineament, Central India (Springer Theses)
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Deep Crustal Structure of the Son-Narmada-Tapti Lineament, Central India (Hardcover)
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Springer-Verlag Berlin and Heidelberg GmbH & Co. KG, Berlin, 2012
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ISBN 13 : 9783642284410
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Hardcover. Etat : new. Hardcover. 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. 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. Shipping may be from multiple locations in the US or from the UK, depending on stock availability. N° de réf. du vendeur 9783642284410
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Deep Crustal Structure of the Son-Narmada-Tapti Lineament, Central India (Springer Theses)
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Deep Crustal Structure of the Son-Narmada-Tapti Lineament, Central India : Doctoral Thesis Accepted Byh the Osmania University, Hyderabad, India
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Springer, 2012
ISBN 10 : 3642284418
ISBN 13 : 9783642284410
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Deep Crustal Structure of the Son-Narmada-Tapti Lineament, Central India (Springer Theses)
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Deep Crustal Structure of the Son-Narmada-Tapti Lineament, Central India : Doctoral Thesis Accepted Byh the Osmania University, Hyderabad, India
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Deep Crustal Structure of the Son-Narmada-Tapti Lineament, Central India
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Springer Berlin Heidelberg, Springer Berlin Heidelberg Apr 2012, 2012
ISBN 10 : 3642284418
ISBN 13 : 9783642284410
Neuf
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Buch. 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. 168 pp. Englisch. N° de réf. du vendeur 9783642284410
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Deep Crustal Structure of the Son-Narmada-Tapti Lineament, Central India : Doctoral Thesis Accepted Byh the Osmania University, Hyderabad, India
Edité par
Springer, 2012
ISBN 10 : 3642284418
ISBN 13 : 9783642284410
Ancien ou d'occasion
Couverture rigide
Vendeur : GreatBookPricesUK, Woodford Green, Royaume-Uni
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Deep Crustal Structure of the Son-narmada-tapti Lineament, Central India
Edité par
Springer-Verlag Berlin and Heidelberg GmbH & Co. KG, 2012
ISBN 10 : 3642284418
ISBN 13 : 9783642284410
Neuf
Couverture rigide
Vendeur : Kennys Bookshop and Art Galleries Ltd., Galway, GY, Irlande
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Etat : New. 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. Series: Springer Theses. Num Pages: 163 pages, 6 black & white illustrations, 85 colour illustrations, biography. BIC Classification: PHVG; RBGD. Category: (P) Professional & Vocational. Dimension: 235 x 155 x 15. Weight in Grams: 421. . 2012. 2012th Edition. hardcover. . . . . N° de réf. du vendeur V9783642284410
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