Cambridge University Press, 2008, 463 с.
Учебник по реологии горных пород, написанный одним из ведущих исследователей в данном направлении. Основной упор сделан на реологию пород при высоких температурах и давлениях, характерных для нижней коры и мантии Земли.
Part I General background. Stress and strain. Thermodynamics. Phenomenological theory of deformation .
Part II Materials science of deformation. Elasticity. Crystalline defects. Experimental techniques for study of plastic deformation. Brittle deformation, brittle-plastic and brittle-ductile transition. Diffusion and diffusional creep. Dislocation creep. Effects of pressure and water. Physical mechanisms of seismic wave attenuation. Deformation of multi-phase materials. Grain size. Lattice-preferred orientation. Effects of phase transformations. Stability and localization of deformation.
Part III Geological and geophysical applications. Composition and structure of Earth's interior. Inference of rheological structure of Earth from time-dependent deformation. Inference of rheological structure of Earth from mineral physics. Heterogeneity of Earth structure and its geodynamic implications.
Учебник по реологии горных пород, написанный одним из ведущих исследователей в данном направлении. Основной упор сделан на реологию пород при высоких температурах и давлениях, характерных для нижней коры и мантии Земли.
Part I General background. Stress and strain. Thermodynamics. Phenomenological theory of deformation .
Part II Materials science of deformation. Elasticity. Crystalline defects. Experimental techniques for study of plastic deformation. Brittle deformation, brittle-plastic and brittle-ductile transition. Diffusion and diffusional creep. Dislocation creep. Effects of pressure and water. Physical mechanisms of seismic wave attenuation. Deformation of multi-phase materials. Grain size. Lattice-preferred orientation. Effects of phase transformations. Stability and localization of deformation.
Part III Geological and geophysical applications. Composition and structure of Earth's interior. Inference of rheological structure of Earth from time-dependent deformation. Inference of rheological structure of Earth from mineral physics. Heterogeneity of Earth structure and its geodynamic implications.