Produktart
Zustand
Einband
Weitere Eigenschaften
Gratisversand
Land des Verkäufers
Verkäuferbewertung
Verlag: Giardini, Italy, 1994
Anbieter: PsychoBabel & Skoob Books, Didcot, Oxfordshire, OXON, Vereinigtes Königreich
paperback. Zustand: Very Good. Zustand des Schutzumschlags: No Dust Jacket. Binding is very well preserved, though with some instances of minor wear to edges and corners. pages are clean and crisp and printing is tight clean and bright throughout. 3 included inserts are in very good condition. Used.
Anbieter: Antiquariat Renner OHG, Albstadt, Deutschland
Verbandsmitglied: BOEV
Verlag: Springer Berlin, 1991
ISBN 10: 3540535640ISBN 13: 9783540535645
Anbieter: ralfs-buecherkiste, Herzfelde, MOL, Deutschland
Buch
Hardcover/ Pappband. Zustand: Gut. 223 S. Guter Zustand/ Good With figures and tables. Ex-Library. Cover mildly used. ha1064048 Sprache: Englisch Gewicht in Gramm: 550.
Verlag: Springer, 1991
ISBN 10: 3540535640ISBN 13: 9783540535645
Anbieter: Buchpark, Trebbin, Deutschland
Buch
Zustand: Sehr gut. Zustand: Sehr gut - Gepflegter, sauberer Zustand. Innen: Seiten eingerissen, Seiten vergilbt. | Seiten: 234.
Verlag: Springer Berlin Heidelberg, 2014
ISBN 10: 3662138522ISBN 13: 9783662138526
Anbieter: AHA-BUCH GmbH, Einbeck, Deutschland
Buch
Taschenbuch. Zustand: Neu. Druck auf Anfrage Neuware - Printed after ordering - In this volume the author gives a detailed presentation of his theory of multiphase mixtures with structure. The book also addresses students, and in addition encourages further research. Based on the concept of averaging the field equations, conservation and balance equations are developed. A material deformation postulate leads to structured mixtures. The resulting model is compared with those in use elsewhere. The final chapters are devoted to constitutive theory and constitutive equations. In particular, two-phase mixtures are treated in some detail.
Verlag: Springer US, 2012
ISBN 10: 1461351758ISBN 13: 9781461351757
Anbieter: AHA-BUCH GmbH, Einbeck, Deutschland
Buch
Taschenbuch. Zustand: Neu. Druck auf Anfrage Neuware - Printed after ordering - Volcanic eruptions are fascinating manifestations of the Earth's dynamic inte rior which has been cooling for the past several billion years. The planets of the solar system originated some 4.5 billion years ago from the same gas and dust cloud created by the big bang. Some of the gas collapsed by the gravitational force to form the Sun at the center, while the whirling disk of gas and dust around the Sun subsequently cooled and lumped together to form larger and larger lumps of materials or planetesimals. These planetesimals collided fre quently and violently and in the process liberated heat that melted the material in them. With time this material gradually cooled and formed the planets of the solar system. During the second half of the twentieth century the theory of plate tectonics of the Earth became established and demonstrated that our planet is covered with six large and many small plates of the lithosphere. These plates move over a highly viscous lower part of the Earth's upper mantle and contain the continental and oceanic crusts. The lower mantle extends below the upper mantle until it meets the core that is more than half the diameter of the entire globe (12,740 km). The inner core consists mostly of iron and its temperature is about 5000 kelvin, whereas the liquid outer core is turbulent, rotates faster than the mantle, consists primarily of iron, and is the source of the Earth's magnetic field.
Verlag: Springer US, 2012
ISBN 10: 1461351758ISBN 13: 9781461351757
Anbieter: moluna, Greven, Deutschland
Buch
Zustand: New.
Verlag: Springer US, 2001
ISBN 10: 0306466252ISBN 13: 9780306466250
Anbieter: moluna, Greven, Deutschland
Buch
Gebunden. Zustand: New.
Verlag: Springer US, 2001
ISBN 10: 0306466252ISBN 13: 9780306466250
Anbieter: AHA-BUCH GmbH, Einbeck, Deutschland
Buch
Buch. Zustand: Neu. Druck auf Anfrage Neuware - Printed after ordering - Volcanic eruptions are fascinating manifestations of the Earth's dynamic inte rior which has been cooling for the past several billion years. The planets of the solar system originated some 4.5 billion years ago from the same gas and dust cloud created by the big bang. Some of the gas collapsed by the gravitational force to form the Sun at the center, while the whirling disk of gas and dust around the Sun subsequently cooled and lumped together to form larger and larger lumps of materials or planetesimals. These planetesimals collided fre quently and violently and in the process liberated heat that melted the material in them. With time this material gradually cooled and formed the planets of the solar system. During the second half of the twentieth century the theory of plate tectonics of the Earth became established and demonstrated that our planet is covered with six large and many small plates of the lithosphere. These plates move over a highly viscous lower part of the Earth's upper mantle and contain the continental and oceanic crusts. The lower mantle extends below the upper mantle until it meets the core that is more than half the diameter of the entire globe (12,740 km). The inner core consists mostly of iron and its temperature is about 5000 kelvin, whereas the liquid outer core is turbulent, rotates faster than the mantle, consists primarily of iron, and is the source of the Earth's magnetic field.