Boschi r (12 Ergebnisse)

- Softcover
Anbieter: libreriauniversitaria.it, Occhiobello, RO, Italienlibreriauniversitaria.it
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Zustand: NEW.

Anbieter: Libreria Piani, Monte San Pietro, BO, ItalienLibreria Piani
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In den WarenkorbTrento, 1976, 8vo stralcio con copertina posticcia muta, pp. 86/113 con 16 illustrazioni fotografiche e 14 piantine. - !! ATTENZIONE !!: Con il termine estratto (o stralcio) intendiamo riferirci ad un fascicolo contenente un articolo, completo in se, sia che esso sia stato stampato a parte utilizzando la stessa composizione sia…che provenga direttamente da una rivista. Le pagine sono indicate come "da/a", ad esempio: 229/231 significa che il testo ?® composto da tre pagine. Quando la rivista di provenienza non viene indicata ? perch? ci ?® sconosciuta. - !! ATTENTION !!: : NOT A BOOK : ?Äúextract?Äù or ?Äúexcerpt?Äù means simply a few pages, original nonetheless, printed in a magazine. Pages are indicated as in "from?Äù ?Äúto", for example: 229/231 means the text comprises three pages (229, 230 and 231). If the magazine that contained the pages is not mentioned, it is because it is unknown to us.

- Hardcover
Anbieter: Better World Books: West, Reno, NV, USABetter World Books: West
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EUR 250,33
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Zustand: Good. Former library copy. Pages intact with minimal writing/highlighting. The binding may be loose and creased. Dust jackets/supplements are not included. Includes library markings. Stock photo provided. Product includes identifying sticker. Better World Books: Buy Books. Do Good.

- Softcover
Anbieter: Buchpark, Trebbin, DeutschlandBuchpark
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EUR 186,96
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Zustand: Sehr gut. Zustand: Sehr gut | Seiten: 728 | Sprache: Englisch | Produktart: Bücher | 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 re…solved 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.

- Softcover
Anbieter: Ria Christie Collections, Uxbridge, Vereinigtes KönigreichRia Christie Collections
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EUR 314,27
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Zustand: New. In.

- Hardcover
Anbieter: Ria Christie Collections, Uxbridge, Vereinigtes KönigreichRia Christie Collections
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Zustand: New. In.

- Softcover
Anbieter: moluna, Greven, Deutschlandmoluna
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EUR 336,82
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Zustand: New. 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, controlling tectonic and dynamic processes such as man.

- Hardcover
Anbieter: AHA-BUCH GmbH, Einbeck, DeutschlandAHA-BUCH GmbH
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EUR 333,77
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Buch. Zustand: 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 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.

Glacial Isostasy, Sea-level and Mantle Rheology
Sabadini, Roberto (Editor)/ Lambeck, K. (Editor)/ Boschi, E. (Editor)
- Softcover
Anbieter: Revaluation Books, Exeter, Vereinigtes KönigreichRevaluation Books
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EUR 457,00
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Paperback. Zustand: Brand New. 728 pages. 9.20x6.00x1.60 inches. In Stock.

- Softcover
Anbieter: AHA-BUCH GmbH, Einbeck, DeutschlandAHA-BUCH GmbH
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EUR 469,00
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Taschenbuch. Zustand: Neu. 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.

- Softcover
Anbieter: Brook Bookstore, Milano, MI, ItalienBrook Bookstore
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EUR 26,08
EUR 47,49 VersandVersand von Italien nach USAAnzahl: 3 verfügbar
Zustand: new.

Sprache: Deutsch
- Hardcover
Anbieter: Antiquariat Bookfarm, Löbnitz, DeutschlandAntiquariat Bookfarm
Verkäufer/-in kontaktierenVerkäufer/-in mit 5 SternenZustand: Gebraucht - Gut
EUR 267,80
EUR 40,00 VersandVersand von Deutschland nach USAAnzahl: 1 verfügbar
In den WarenkorbHardcover. Zustand: Gut. Ehem. Bibliotheksexemplar mit Signatur und Stempel. GUTER Zustand, ein paar Gebrauchsspuren. Ex-library with stamp and library-signature. GOOD condition, some traces of use. AB-8160 Sprache: Deutsch Gewicht in Gramm: 1550.