9783844397567 - earth crustal modelling: geodetic applications of the vening meinesz-mortiz hypothesis de bagherbandi, mohammad; e. sjöberg, lars (6 resultados)
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Taschenbuch. Condición: Neu. Earth Crustal Modelling | Geodetic applications of the Vening Meinesz-Mortiz hypothesis | Mohammad Bagherbandi (u. a.) | Taschenbuch | 228 S. | Englisch | 2011 | LAP LAMBERT Academic Publishing | EAN 9783844397567 | Verantwortliche Person für die EU: BoD - Books on Demand, In de Tarpen 42, 22848 Nord…erstedt, info[at]bod[dot]de | Anbieter: preigu.
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Librería: BuchWeltWeit Ludwig Meier e.K., Bergisch Gladbach, AlemaniaBuchWeltWeit Ludwig Meier e.K.
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Taschenbuch. Condición: Neu. This item is printed on demand - it takes 3-4 days longer - Neuware -This book presents a gravimetric-isostatic model to determine the Earth's crustal thickness and its geodetic applications, which is great interest for geoscientists. The main reasons for studying an isostatic model are on one hand t…he gaps and uncertainties of the seismic models, and, on the other hand, the generous availability of gravity data from global models for the gravimetric-isostatic model. In this study, we present a new gravimetric- isostatic Moho model, called the Vening Meinesz- Moritz (VMM) model. The application of the VMM Moho model could be in estimating the Moho density contrast, studying the dynamics of the mantle or studying the deep-seated inhomogeneities of the Earth's mantle by gravity field analysis, smoothing the gravity field for downward continuation of the gravity field from the above surface of the Earth (from satellite mission e.g. GOCE) to the mean sea level. 228 pp. Englisch.
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Condición: New. Dieser Artikel ist ein Print on Demand Artikel und wird nach Ihrer Bestellung fuer Sie gedruckt. Autor/Autorin: Bagherbandi MohammadMohammad Bagherbandi, 1977, PhD in Geodesy from KTH in Stockholm. He is working on Moho determination and other dynamic-isostatic effects. Lars E. Sjoeberg, 1947, is professor of Geo…desy at KTH since 1984 with.
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Librería: buchversandmimpf2000, Emtmannsberg, BAYE, Alemaniabuchversandmimpf2000
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Taschenbuch. Condición: Neu. This item is printed on demand - Print on Demand Titel. Neuware -This book presents a gravimetric-isostatic model to determine the Earth's crustal thickness and its geodetic applications, which is great interest for geoscientists. The main reasons for studying an isostatic model are on one hand the g…aps and uncertainties of the seismic models, and, on the other hand, the generous availability of gravity data from global models for the gravimetric-isostatic model. In this study, we present a new gravimetric- isostatic Moho model, called the Vening Meinesz- Moritz (VMM) model. The application of the VMM Moho model could be in estimating the Moho density contrast, studying the dynamics of the mantle or studying the deep-seated inhomogeneities of the Earth's mantle by gravity field analysis, smoothing the gravity field for downward continuation of the gravity field from the above surface of the Earth (from satellite mission e.g. GOCE) to the mean sea level.VDM Verlag, Dudweiler Landstraße 99, 66123 Saarbrücken 228 pp. Englisch.
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Librería: AHA-BUCH GmbH, Einbeck, AlemaniaAHA-BUCH GmbH
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Taschenbuch. Condición: Neu. nach der Bestellung gedruckt Neuware - Printed after ordering - This book presents a gravimetric-isostatic model to determine the Earth's crustal thickness and its geodetic applications, which is great interest for geoscientists. The main reasons for studying an isostatic model are on one hand the ga…ps and uncertainties of the seismic models, and, on the other hand, the generous availability of gravity data from global models for the gravimetric-isostatic model. In this study, we present a new gravimetric- isostatic Moho model, called the Vening Meinesz- Moritz (VMM) model. The application of the VMM Moho model could be in estimating the Moho density contrast, studying the dynamics of the mantle or studying the deep-seated inhomogeneities of the Earth's mantle by gravity field analysis, smoothing the gravity field for downward continuation of the gravity field from the above surface of the Earth (from satellite mission e.g. GOCE) to the mean sea level.
