Sprache: Englisch
Verlag: CreateSpace Independent Publishing Platform (edition 1), 2013
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Anbieter: Antiquariat Bookfarm, Löbnitz, Deutschland
Hardcover. XIII, 484 S. Ehem. Bibliotheksexemplar mit Signatur und Stempel. GUTER Zustand, ein paar Gebrauchsspuren. Ex-library with stamp and library-signature. GOOD condition, some traces of use. w09690 3540532730 Sprache: Englisch Gewicht in Gramm: 1100.
Sprache: Englisch
Verlag: Creative Media Partners, LLC Sep 2021, 2021
ISBN 10: 1014235529 ISBN 13: 9781014235527
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Sprache: Englisch
Verlag: Springer Berlin Heidelberg, 2014
ISBN 10: 364276147X ISBN 13: 9783642761478
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Zustand: New. Describes principles in muscle metabolism, meat quality and meat safety using case studies Discusses the microbial safety of meat products, primary pathogens of concern, and pathogen detection Offers solutions on how to control ba.
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Taschenbuch. Zustand: Neu. Equilibrium and Kinetics in Contact Metamorphism | The Ballachulish Igneous Complex and Its Aureole | Gerhard Voll (u. a.) | Taschenbuch | xiii | Englisch | 2014 | Springer | EAN 9783642761478 | Verantwortliche Person für die EU: Springer Verlag GmbH, Tiergartenstr. 17, 69121 Heidelberg, juergen[dot]hartmann[at]springer[dot]com | Anbieter: preigu.
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In den WarenkorbPaperback. Zustand: Brand New. 512 pages. 9.60x6.70x1.20 inches. In Stock.
Sprache: Englisch
Verlag: Springer Berlin Heidelberg, 2014
ISBN 10: 364276147X ISBN 13: 9783642761478
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Taschenbuch. Zustand: Neu. Druck auf Anfrage Neuware - Printed after ordering - With the new global tectonics approach in the Earth Sciences, the quan titative aspects of the dynamics of rock-forming processes came into focus: geologists are no longer satisfied knowing the pressure-tempera ture conditions of the formation of a metamorphic rock or of the emplace ment of a magmatic body, but instead would like to learn the time history of these rocks as well, i. e. , derive the temperature-pressure-time path and relate it to a tectonic process. To achieve this goal, a knowledge of both pressure-temperature-dependent equilibria and the time scales at which these equilibria may be attained are essential. However, the latter kinetic information is much more difficult to retrieve than that on equilibria: whereas equilibria are controlled by state variables, and proper laboratory experiments may be directly applied to equilibrium natural assemblages, kinetics also depends on factors other than state variables, such as grain size, dislocation density, and especially time (rate of heating, duration of annealing, rate of cooling). Extrapolation of kinetic data obtained at high temperatures on laboratory time scales to more realistic lower tempera tures and geological time scales are dangerous because, for example, of possible changes from an intrinsically controlled defect regime to an extrinsic one as temperature is lowered, or from an interface-controlled to a diffusion-controlled reaction mechanism.