2000 | OriginalPaper | Buchkapitel
Poro — Thermo — Elasticity of Rocks
verfasst von : Professor Dr. Georg Mandl
Erschienen in: Faulting in Brittle Rocks
Verlag: Springer Berlin Heidelberg
Enthalten in: Professional Book Archive
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Small elastic strains precede the formation of tensile fractures and the inelastic straining that leads to the formation of faults and folds in the brittle crust. Small elastic strains also occur in the propagation of acoustic waves, in earthquakes, in erosive unloading of rocks, during changes in pore pressure and temperature, and during the geometrical adjustment of sliding fault blocks.