Record Display for the EPA National Library Catalog

RECORD NUMBER: 574 OF 1770

Main Title Geodynamics of the Lithosphere An Introduction / [electronic resource] :
Type EBOOK
Author Stüwe, Kurt.
Publisher Springer Berlin Heidelberg,
Year Published 2007
Call Number QC801-809
ISBN 9783540712374
Subjects Geology ; Physical geography ; Computer science--Mathematics ; Thermodynamics
Internet Access
Description Access URL
http://dx.doi.org/10.1007/978-3-540-71237-4
Edition Second Edition.
Collation XIV, 493 p. online resource.
Notes
Due to license restrictions, this resource is available to EPA employees and authorized contractors only
Contents Notes
Plate Tectonics -- Energetics: Heat and Temperature -- Kinematics: Morphology and Deformation -- Mechanics: Force and Rheology -- Dynamic Processes -- Metamorphic Processes. 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. 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.