The large scale structure of the earth is caused by geodynamic processes which are explained using energetic, kinematic and dynamic descriptions. While "geodynamic processes" are understood to include a large variety of processes and the term is used quite loosely, the methods of their description involve well defined fields. Energetic descriptions are involved with distribu tion of energy in our planet, typically expressed in terms of heat and tempera ture. Kinematic descriptions describe movements using velocities, strains and strain rates. Dynamic descriptions indicate how stresses and forces behave. In the field, we document only the consequences of geological processes. The underlying causes are much harder to constrain directly. Nevertheless, if we want to explain the tectonic evolution of our planet, we need to interpret these causes or: "driving forces" . For this, we need to find a dynamic description of geological processes that is consistent with our observations. Our descriptions relate causes and consequences - tectonic processes with field observations. In many cases, we will use equations as a concise form to describe processes and observations in nature. As we will be dealing mostly with large scale tectonic questions, the observations that we shall use are also on a large scale. For example, we shall use observations on the elevation (Fig. 1. 1) and heat flow of mountain ranges, the thickness of continents and the water depth of the oceans.
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Buch. Zustand: Neu. This item is printed on demand - it takes 3-4 days longer - Neuware -This book is an introductory text for all earth scientists interested in learning about the quantitative description of geological problems. It contains chapters on heat flow, sedimentary basin modelling, mechanics of continental deformation, PT path modelling, geomorphology and mass transfer and more. In its style, the book is aimed at the field oriented geologist that wants to begin with learning about the quantitative description of problems. Graduate students and scientists will find the book a good starting point for a quantitative treatment of their data. The new edition, revised and extended, features even more illustrations and maps, about 100 corrections of scientific problems, improvement of geomorphology section and shortening of several sections which obviously are too complicated. Update and modernisation of several sections, for example the section on pressure and updated references. 508 pp. Englisch. Bestandsnummer des Verkäufers 9783540712367
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Zustand: New. Dieser Artikel ist ein Print on Demand Artikel und wird nach Ihrer Bestellung fuer Sie gedruckt. Clear representation of the subject for the field oriented geologistArtwork specially designed for this bookQualitative representation of geodynamical processesThis second edition of the important introductory text for earth scie. Bestandsnummer des Verkäufers 4899179
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Buch. Zustand: Neu. Geodynamics of the Lithosphere | An Introduction | Kurt Stüwe | Buch | xiv | Englisch | 2007 | Springer | EAN 9783540712367 | Verantwortliche Person für die EU: Springer Verlag GmbH, Tiergartenstr. 17, 69121 Heidelberg, juergen[dot]hartmann[at]springer[dot]com | Anbieter: preigu Print on Demand. Bestandsnummer des Verkäufers 102066352
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Buch. Zustand: Neu. This item is printed on demand - Print on Demand Titel. Neuware -This book is an introductory text for all earth scientists interested in learning about the quantitative description of geological problems. In its style, the book is aimed at the field oriented geologist that wants to begin with learning about the quantitative description of problems. The new edition, revised and extended, features even more illustrations and maps, about 100 corrections of scientific problems, improvement of geomorphology section and shortening of several sections which obviously are too complicated. Graduate students and scientists will find the book a good starting point for a quantitative treatment of their data.Springer-Verlag KG, Sachsenplatz 4-6, 1201 Wien 508 pp. Englisch. Bestandsnummer des Verkäufers 9783540712367
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Buch. Zustand: Neu. Druck auf Anfrage Neuware - Printed after ordering - The large scale structure of the earth is caused by geodynamic processes which are explained using energetic, kinematic and dynamic descriptions. While 'geodynamic processes' are understood to include a large variety of processes and the term is used quite loosely, the methods of their description involve well defined fields. Energetic descriptions are involved with distribu tion of energy in our planet, typically expressed in terms of heat and tempera ture. Kinematic descriptions describe movements using velocities, strains and strain rates. Dynamic descriptions indicate how stresses and forces behave. In the field, we document only the consequences of geological processes. The underlying causes are much harder to constrain directly. Nevertheless, if we want to explain the tectonic evolution of our planet, we need to interpret these causes or: 'driving forces' . For this, we need to find a dynamic description of geological processes that is consistent with our observations. Our descriptions relate causes and consequences - tectonic processes with field observations. In many cases, we will use equations as a concise form to describe processes and observations in nature. As we will be dealing mostly with large scale tectonic questions, the observations that we shall use are also on a large scale. For example, we shall use observations on the elevation (Fig. 1. 1) and heat flow of mountain ranges, the thickness of continents and the water depth of the oceans. Bestandsnummer des Verkäufers 9783540712367
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