Abstract
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 distribution of energy in our planet, typically expressed in terms of heat and temperature. Kinematic descriptions describe movements using velocities, strains and strain rates. Dynamic descriptions indicate how stresses and forces behave.
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© 2007 Springer-Verlag Berlin Heidelberg
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(2007). Introduction. In: Geodynamics of the Lithosphere. Springer, Berlin, Heidelberg. https://doi.org/10.1007/978-3-540-71237-4_1
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DOI: https://doi.org/10.1007/978-3-540-71237-4_1
Publisher Name: Springer, Berlin, Heidelberg
Print ISBN: 978-3-540-71236-7
Online ISBN: 978-3-540-71237-4
eBook Packages: Earth and Environmental ScienceEarth and Environmental Science (R0)