Titlebook: Metamorphic Reactions; Kinetics, Textures, Alan Bruce Thompson,David C. Rubie Book 1985 Springer-Verlag New York, Inc. 1985 Reactions.crys

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The Influence of Defect Crystallography on Some Properties of Orthosilicates,ee that is a function of the metamorphic and deformation history. Dislocation creep of some kind is undoubtedly the controlling mechanism for accommodating large plastic strains at sufficiently high temperatures and pressures (see Kirby, 1983, and references therein), and recent electron microscopy

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A Natural Example of the Kinetic Controls of Compositional and Textural Equilibration,llister, 1969; Loomis, 1976). However, the significance of kinetics in controlling assemblages, compositions, and textures has been treated by relatively few authors (e.g., Loomis, 1976; Foster, 1982). Among the variables that control the rates of metamorphic reactions are the rate of supply (or rem

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On the Relationship between Deformation and Metamorphism, with Special Reference to the Behavior ofthe subject, there has never been a completely satisfactory understanding of the interrelationships at the mechanistic level. The literature abounds with descriptions of mineralogical changes that mirror the intensity of strain in heterogeneously deformed rocks (e.g., Teall, 1885; Beach, 1973; Kerri

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Heterogeneous Deformation, Foliation Development, and Metamorphic Processes in a Polyphase Myloniteveloped in tectonites. Mineral changes that accompany deformation may exert an important influence on the rheological behavior of rocks, and deformation processes play a significant role in the mechanisms of mineral reactions that take place in a deforming aggregate (White and Knipe, 1978; Brodie an

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nugatory

The Possible Effects of Deformation on Chemical Processes in Metamorphic Fault Zones,of foliation development (hornfels and granofels versus slate, phyllite, schist, and gneiss) and in the modification of textures during syntectonic mineral growth (e.g., Misch, 1969; Rosenfeld, 1970). The influence of deformation on chemical aspects of petrology is less fully explored but is evident

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Deformation with Simultaneous Chemical Change: The Thermodynamic Basis,ostatic stress, the chemical potential of a component at a point in the material has a range of values according to which plane in the material one considers. The idea that the normal compressive stress on a plane has this kind of variability has long been accepted; here it is proposed that the chem

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