Titlebook: Geodynamics of the Lithosphere; Kurt Stüwe Textbook 20021st edition Springer-Verlag Berlin Heidelberg 2002 Approximation.Deformation.Litho

Plaque

Heat and Temperature, equivalent to mass × velocity. (1 J =1 kg m.s.), or volume × pressure (1 J = 1 m. × Pa = 1 N m). These conversions give us a first indication that thermal and mechanical energy are often hard to separate. Thermal energy may be converted into temperature using heat capacity and density which are par

駁船

慎重

Force and Rheology,rogens, provide a useful independent constraint on models based on field observations. Let us consider an example: A field geologist finds in a Precambrian shield folds and thrusts that he interprets to have formed as the consequence of crustal shortening. A detailed strain analysis shows that 80% s

毀壞

glamor

,-,-,-,-Paths,sure ., 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

反對

Bestimmung der Festhaltungskraftageneses or the mechanisms with which rocks deform. These and many other examples are parameters relevant for orogenic processes andan understanding of the thermal structure of the lithosphere is therefore crucial for the understanding of most geodynamic processes.

通情達理

哀求

咆哮

Monocle

geodynamical processesThe 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 by earth scientists quite l