Titlebook: Geodynamics of the Lithosphere; An Introduction Kurt Stüwe Textbook 2007Latest edition Springer-Verlag Berlin Heidelberg 2007 Deformation.G

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https://doi.org/10.1007/978-3-662-31482-1nic model is presented and some basic principles how to describe it are discussed. Some arguments that suggest why plate tectonics may . work are also presented. In the second part of this chapter we discuss the layered structure of the earth and the geographic distribution of lithospheric plates. W

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Luhmann as Analytical Strategiststrain and ventures therefore a bit into the field of structural geology. However, mostly we shall discuss processes like the elevation of mountain ranges, and the depth of the oceans, as well as the . of such parameters: kinematics. We begin with a consideration of the basics of strain. Our summary

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https://doi.org/10.1007/978-3-662-28959-4sure ., temperature . and deformation . that the rocks experienced: the metamorphic evolution of the rocks. Data on the metamorphic evolution are particularly important when interpreting ancient orogens where it is impossible to measure many other parameters directly (e.g. surface elevation, surface

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https://doi.org/10.1007/978-3-663-08082-4ng point in geodynamics, as so many properties of rocks that may be observed in the field are a strong function of temperature, for example the formation of metamorphic parageneses or the mechanisms with which rocks deform.

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Die Microsoft Programmer’s Workbenchtwo thirds of this chapter are dedicated to the description of continents in extension and in collision. In the last third of this chapter we touch upon a range of interesting and currently very topical geodynamic problems.