Titlebook: Deformation Processes in Minerals, Ceramics and Rocks; David J. Barber,Philip G. Meredith Book 1990 D. J. Barber, P. G. Meredith & contrib

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Jozef Rovensky,Juraj Payer,Manfred Herold to engineering structures or to mechanics of the Earth’s crust). This arises in part from an emphasis on phenomenological aspects of macroscopic deformation and failure at the expense of micromechanical aspects of fracture, and in part from the rate, size, and environment dependence of the brittle

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Jozef Rovensky,Juraj Payer,Manfred Heroldopic level (Lawn & Wilshaw 1975, Section 3.3). Macroscopic behaviour is to be interpreted in terms of microscopic processes. As far as cracks are concerned, important microscopic processes are nucleation and propagation of extensional cracks. However, in order to take into account the fact that a re

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Jozef Rovensky,Juraj Payer,Manfred Heroldee are the three classes of metals with cubic crystal structures — f.c.c., b.c.c, and h.c.p.), showing a progression of plastic flow properties (Frost & Ashby 1982, Tables 18.3 & 18.4) and of cleavage properties (Kelly, Tyson & Cottrell 1967; Gandhi & Ashby 1979, Table 4 & Fig. 28). These are illust

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https://doi.org/10.1007/978-94-011-2294-8aws are adequate to describe the diffusion-controlled plastic deformation (e.g. Karato .. 1986), they do not take account of plastic anisotropy due to slip. We attempt to introduce a generalized description of anisotropic plastic flow of olivine based on polycrystal plasticity theory which takes int

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https://doi.org/10.1007/978-94-011-2294-8n deformed marcasite (Fagot .. 1981), and has provided detailed information on the ductile behaviour of pyrite (Cox .. 1981, Graf .. 1981, Levade .. 1982) and sphalerite (Levade .. 1986). Previous interpretations of the flow mechanisms in experimentally deformed polycrystalline chalcopyrite resulted

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Deformation Processes in Minerals, Ceramics and Rocks