9780792311676 - glacial isostasy, sea-level and mantle rheology: proceedings of the nato advanced research workshop on glacial isostasy, sea-level, and mantle rheo: 334 (nato science series c:, 334) (12 resultados)
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Glacial Isostasy, Sea-Level, and Mantle Rheology : Proceedings of the NATO Advanced Research Workshop on Glacial Isostasy, Sea-Level, and Mantle Rheo
NATO Advanced Research Workshop on Glacial Isostasy, Sea-level, and Mantle Rheology (1990 : Erice, Italy) (COR); Lambeck, Kurt; Boschi, E. (EDT); Sabadini, Roberto; Boschi, E.; North Atlantic Treaty Organization. Scientific Affairs Division (COR)
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Glacial Isostasy, Sea-Level, and Mantle Rheology : Proceedings of the NATO Advanced Research Workshop on Glacial Isostasy, Sea-Level, and Mantle Rheo
NATO Advanced Research Workshop on Glacial Isostasy, Sea-level, and Mantle Rheology (1990 : Erice, Italy) (COR); Lambeck, Kurt; Boschi, E. (EDT); Sabadini, Roberto; Boschi, E.; North Atlantic Treaty Organization. Scientific Affairs Division (COR)
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Glacial Isostasy, Sea-Level, and Mantle Rheology : Proceedings of the NATO Advanced Research Workshop on Glacial Isostasy, Sea-Level, and Mantle Rheo
NATO Advanced Research Workshop on Glacial Isostasy, Sea-level, and Mantle Rheology (1990 : Erice, Italy) (COR); Lambeck, Kurt; Boschi, E. (EDT); Sabadini, Roberto; Boschi, E.; North Atlantic Treaty Organization. Scientific Affairs Division (COR)
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Glacial Isostasy, Sea-Level, and Mantle Rheology : Proceedings of the NATO Advanced Research Workshop on Glacial Isostasy, Sea-Level, and Mantle Rheo
NATO Advanced Research Workshop on Glacial Isostasy, Sea-level, and Mantle Rheology (1990 : Erice, Italy) (COR); Lambeck, Kurt; Boschi, E. (EDT); Sabadini, Roberto; Boschi, E.; North Atlantic Treaty Organization. Scientific Affairs Division (COR)
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Buch. Condición: Neu. Druck auf Anfrage Neuware - Printed after ordering - by K. Lambeck, R. Sabadini and E. B08Chi Viscosity is one of the important material properties of the Earth, controlling tectonic and dynamic processes such as mantle convection, isostasy, and glacial rebound. Yet it remains a poorly resolved parameter an…d basic questions such as whether the planet's response to loading is linear or non-linear, or what are its depth and lateral variations remain uncertain. Part of the answer to such questions lies in laboratory observations of the rheology of terrestrial materials. But the extrapolation of such measurements from the laboratory environment to the geological environment is a hazardous and vexing undertaking, for neither the time scales nor the strain rates characterizing the geological processes can be reproduced in the laboratory. General rules for this extrapolation are that if deformation is observed in the laboratory at a particular temperature, deformation in geological environments will occur at a much reduced temperature, and thatif at laboratory strain rates a particular deformation mechanism dominates over all others, the relative importance of possible mechanisms may be quite different at the geologically encountered strain rates. Hence experimental results are little more than guidelines as to how the Earth may respond to forces on long time scales.
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Gebunden. Condición: New. Dieser Artikel ist ein Print on Demand Artikel und wird nach Ihrer Bestellung fuer Sie gedruckt. Proceedings of the NATO Advanced Research Workshop, Erice, Italy, July 27-August 4, 1990 by K. Lambeck, R. Sabadini and E. B08Chi Viscosity is one of the important material properties of the Earth, controlli…ng tectonic and dynamic processes such as man.
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Buch. Condición: Neu. Glacial Isostasy, Sea-Level and Mantle Rheology | R. Sabadini (u. a.) | Buch | Einband - fest (Hardcover) | Englisch | 1991 | Springer Netherland | EAN 9780792311676 | Verantwortliche Person für die EU: Springer Netherlands, Haberstr. 7, 69126 Heidelberg, buchhandel-buch[at]springer[dot]com | Anbieter: prei…gu Print on Demand.
Idioma: Inglés
Editorial: Springer Netherlands, Springer Netherlands Mär 1991, 1991
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Buch. Condición: Neu. This item is printed on demand - Print on Demand Titel. Neuware -by K. Lambeck, R. Sabadini and E. B08Chi Viscosity is one of the important material properties of the Earth, controlling tectonic and dynamic processes such as mantle convection, isostasy, and glacial rebound. Yet it remains a poorly resolved…parameter and basic questions such as whether the planet's response to loading is linear or non-linear, or what are its depth and lateral variations remain uncertain. Part of the answer to such questions lies in laboratory observations of the rheology of terrestrial materials. But the extrapolation of such measurements from the laboratory environment to the geological environment is a hazardous and vexing undertaking, for neither the time scales nor the strain rates characterizing the geological processes can be reproduced in the laboratory. General rules for this extrapolation are that if deformation is observed in the laboratory at a particular temperature, deformation in geological environments will occur at a much reduced temperature, and thatif at laboratory strain rates a particular deformation mechanism dominates over all others, the relative importance of possible mechanisms may be quite different at the geologically encountered strain rates. Hence experimental results are little more than guidelines as to how the Earth may respond to forces on long time scales.Springer Verlag GmbH, Tiergartenstr. 17, 69121 Heidelberg 728 pp. Englisch.
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Buch. Condición: Neu. This item is printed on demand - it takes 3-4 days longer - Neuware -by K. Lambeck, R. Sabadini and E. B08Chi Viscosity is one of the important material properties of the Earth, controlling tectonic and dynamic processes such as mantle convection, isostasy, and glacial rebound. Yet it remains a poorly resol…ved parameter and basic questions such as whether the planet's response to loading is linear or non-linear, or what are its depth and lateral variations remain uncertain. Part of the answer to such questions lies in laboratory observations of the rheology of terrestrial materials. But the extrapolation of such measurements from the laboratory environment to the geological environment is a hazardous and vexing undertaking, for neither the time scales nor the strain rates characterizing the geological processes can be reproduced in the laboratory. General rules for this extrapolation are that if deformation is observed in the laboratory at a particular temperature, deformation in geological environments will occur at a much reduced temperature, and that if at laboratory strain rates a particular deformation mechanism dominates over all others, the relative importance of possible mechanisms may be quite different at the geologically encountered strain rates. Hence experimental results are little more than guidelines as to how the Earth may respond to forces on long time scales. 728 pp. Englisch.
