The northward movement of the Indo-Pakistan plate consumed the Neo-Tethys Ocean. As a result the Indo- Pakistan plate collided with Eurasian plate. During this convergence the Himalayan fold-thrust belt developed due to tectonic loading and thrusting. The Salt Range and the Potwar Plateau (SR/PP) comprise of an east-west trending fold-belt, located in the western deformed portion of the Himalayan fold- thrust belt, N. Pakistan. This research investigate the structural evolution of the SR/PP by analog scale modelling using the centrifuge technique. The foreland sequence of the SR/PP is constructed of layers of plasticine and silicone putty of controlled thickness ratios, and shortened horizontally to replicate the initiation and progressive growth of folds and thrust faults in the study area. The main aim of this research is to resolve the controversy of variation in the structural styles in the SR/PP. This study will also expand the understanding of the structural style in the SR/PP by documenting the progressive evolution of geological structures that develop in centrifuge models and comparing these with the prototype (SR/PP).
Les informations fournies dans la section « Synopsis » peuvent faire référence à une autre édition de ce titre.
The northward movement of the Indo-Pakistan plate consumed the Neo-Tethys Ocean. As a result the Indo- Pakistan plate collided with Eurasian plate. During this convergence the Himalayan fold-thrust belt developed due to tectonic loading and thrusting. The Salt Range and the Potwar Plateau (SR/PP) comprise of an east-west trending fold-belt, located in the western deformed portion of the Himalayan fold- thrust belt, N. Pakistan. This research investigate the structural evolution of the SR/PP by analog scale modelling using the centrifuge technique. The foreland sequence of the SR/PP is constructed of layers of plasticine and silicone putty of controlled thickness ratios, and shortened horizontally to replicate the initiation and progressive growth of folds and thrust faults in the study area. The main aim of this research is to resolve the controversy of variation in the structural styles in the SR/PP. This study will also expand the understanding of the structural style in the SR/PP by documenting the progressive evolution of geological structures that develop in centrifuge models and comparing these with the prototype (SR/PP).
Shah Faisal is working as a Research Associate at the National Centre of Excellence in Geology University of Peshawar, Pakistan. He obtained M.Phil. and M.Sc. degrees in Geology from University of Peshawar, Pakistan. He has also received an M.Sc. degree in Structural Geology from Queen's University, Kingsotn, Ontario, Canada.
Les informations fournies dans la section « A propos du livre » peuvent faire référence à une autre édition de ce titre.
Vendeur : BuchWeltWeit Ludwig Meier e.K., Bergisch Gladbach, Allemagne
Taschenbuch. Etat : Neu. This item is printed on demand - it takes 3-4 days longer - Neuware -The northward movement of the Indo-Pakistan plate consumed the Neo-Tethys Ocean. As a result the Indo- Pakistan plate collided with Eurasian plate. During this convergence the Himalayan fold-thrust belt developed due to tectonic loading and thrusting. The Salt Range and the Potwar Plateau (SR/PP) comprise of an east-west trending fold-belt, located in the western deformed portion of the Himalayan fold- thrust belt, N. Pakistan. This research investigate the structural evolution of the SR/PP by analog scale modelling using the centrifuge technique. The foreland sequence of the SR/PP is constructed of layers of plasticine and silicone putty of controlled thickness ratios, and shortened horizontally to replicate the initiation and progressive growth of folds and thrust faults in the study area. The main aim of this research is to resolve the controversy of variation in the structural styles in the SR/PP. This study will also expand the understanding of the structural style in the SR/PP by documenting the progressive evolution of geological structures that develop in centrifuge models and comparing these with the prototype (SR/PP). 212 pp. Englisch. N° de réf. du vendeur 9783843366236
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Etat : New. Dieser Artikel ist ein Print on Demand Artikel und wird nach Ihrer Bestellung fuer Sie gedruckt. Autor/Autorin: Faisal ShahShah Faisal is working as a Research Associate at the National Centre of Excellence in Geology University of Peshawar, Pakistan. He obtained M.Phil. and M.Sc. degrees in Geology from University of Peshawar, Pakistan. He. N° de réf. du vendeur 5466566
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Taschenbuch. Etat : Neu. nach der Bestellung gedruckt Neuware - Printed after ordering - The northward movement of the Indo-Pakistan plate consumed the Neo-Tethys Ocean. As a result the Indo- Pakistan plate collided with Eurasian plate. During this convergence the Himalayan fold-thrust belt developed due to tectonic loading and thrusting. The Salt Range and the Potwar Plateau (SR/PP) comprise of an east-west trending fold-belt, located in the western deformed portion of the Himalayan fold- thrust belt, N. Pakistan. This research investigate the structural evolution of the SR/PP by analog scale modelling using the centrifuge technique. The foreland sequence of the SR/PP is constructed of layers of plasticine and silicone putty of controlled thickness ratios, and shortened horizontally to replicate the initiation and progressive growth of folds and thrust faults in the study area. The main aim of this research is to resolve the controversy of variation in the structural styles in the SR/PP. This study will also expand the understanding of the structural style in the SR/PP by documenting the progressive evolution of geological structures that develop in centrifuge models and comparing these with the prototype (SR/PP). N° de réf. du vendeur 9783843366236
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Taschenbuch. Etat : Neu. Centrifuge Modelling of the Salt Range and the Potwar Plateau-Pakistan | Contrasting Deformation Styles both along and across the Strike | Shah Faisal | Taschenbuch | 212 S. | Englisch | 2010 | LAP LAMBERT Academic Publishing | EAN 9783843366236 | Verantwortliche Person für die EU: BoD - Books on Demand, In de Tarpen 42, 22848 Norderstedt, info[at]bod[dot]de | Anbieter: preigu. N° de réf. du vendeur 107243781
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Taschenbuch. Etat : Neu. This item is printed on demand - Print on Demand Titel. Neuware -The northward movement of the Indo-Pakistan plate consumed the Neo-Tethys Ocean. As a result the Indo- Pakistan plate collided with Eurasian plate. During this convergence the Himalayan fold-thrust belt developed due to tectonic loading and thrusting. The Salt Range and the Potwar Plateau (SR/PP) comprise of an east-west trending fold-belt, located in the western deformed portion of the Himalayan fold- thrust belt, N. Pakistan. This research investigate the structural evolution of the SR/PP by analog scale modelling using the centrifuge technique. The foreland sequence of the SR/PP is constructed of layers of plasticine and silicone putty of controlled thickness ratios, and shortened horizontally to replicate the initiation and progressive growth of folds and thrust faults in the study area. The main aim of this research is to resolve the controversy of variation in the structural styles in the SR/PP. This study will also expand the understanding of the structural style in the SR/PP by documenting the progressive evolution of geological structures that develop in centrifuge models and comparing these with the prototype (SR/PP).VDM Verlag, Dudweiler Landstraße 99, 66123 Saarbrücken 212 pp. Englisch. N° de réf. du vendeur 9783843366236
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