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This work details the chemical changes that occur in deforming materials subjected to unequal compressions. While thermodynamics provides, at the macroscopic level, an excellent means of understanding & predicting the behaviour of materials in equilibrium & non-equilibrium states, much less is understood about nonhydrostatic stress & interdiffusion at the chemical level. Little is known, for example, about the chemistry of a state resulting from a cylinder of deforming material being more strongly compressed along its length than radially, a state of non-equilibrium that remains no matter how ideal the cylinder's condition in other respects. M. Brian Bayly here provides the outline of a comprehensive approach to gaining a simplified & unified understanding of such phenomena.
Deformations (Mechanics) --- Chemical equilibrium. --- Elastic solids --- Mechanics --- Rheology --- Strains and stresses --- Structural failures --- Equilibrium, Chemical --- Chemistry, Physical and theoretical --- Phase rule and equilibrium --- Geochemistry. --- Materials --- Chemical composition of the earth --- Chemical geology --- Geological chemistry --- Geology, Chemical --- Chemistry --- Earth sciences --- Compression strength testing of materials --- Compression testing of materials --- Compressive strength testing of materials --- Compressive testing of materials --- Compression testing. --- Testing
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Petrology --- Pétrographie --- Pétrologie --- Sédiment --- Sediment --- Pétrographie --- Sediment. --- SEDIMENTOLOGIE --- DIAGENESE ET METASOMATOSE --- PETROLOGIE DE TOUTES LES ROCHES --- GEOPHYSIQUE --- STRUCTURE INTERNE
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Metamorphic rocks --- Petrofabric analysis --- #Hist.Geol. --- Rocks, Metamorphic --- Atlases. --- #Hist.Geol --- Metamorphic rocks - Atlases --- Petrofabric analysis - Atlases --- Rock cleavage --- Metamorphic rock fabric --- TECTONIQUE --- TECTONIQUE DETAIL --- MICROTECTONIQUE --- PETROLOGIE ROCHES METAMORPHIQUES --- STRUCTURE
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