By David J. Barber, Philip G. Meredith (auth.)
This monograph has its origins in a two-day assembly with an analogous identify held in London, England within the spring of 1987. the belief for the assembly got here from contributors of the united kingdom Mineral and Rock Physics staff. It was once held less than the auspices of, and made attainable via the beneficiant aid of, the Mineralogical Society of serious Britain and eire. extra monetary suggestions used to be supplied via ECC overseas pIc and the Cookson crew pIc. The goals of the London assembly have been to survey the present country of data approximately deformation methods in non-metallic fabrics and to compile either specialists and not more skilled Earth scientists and ceramicists who in general had little touch yet shared universal pursuits in deformation mechanisms. This monograph has comparable goals and, certainly, so much of its authors have been keynote audio system on the assembly. accordingly, lots of the contributions comprise a overview point as well as the presentation and dialogue of recent effects. In adopting this structure, the editors wish that the monograph will supply a useful state of the art sourcebook, either to energetic researchers and in addition to graduate scholars simply beginning within the appropriate fields.
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Extra resources for Deformation Processes in Minerals, Ceramics and Rocks
This is likely to be an iterative process that will require input from the techniques that indirectly monitor damage development during progressive deformation. Acknowledgements I should like to take this opportunity to thank Barry Atkinson for enthusiastically introducing me to fracture in rocks and minerals, and for sharing a number of years of very enjoyable collaborative research. Stan Murrell, Peter Sammonds and Ian Main are thanked for many helpful and constructive comments on earlier drafts of this overview.
Two major restrictions are implicit in this classical Griffith approach. First, it is assumed that all cracks are open and, second, it is assumed that no internal pressure (such as a pore fluid pressure) acts within the cracks. In reality, both 24 P. O. MEREDITH of these assumptions are commonly violated. The application of even a modest confining pressure will tend to close cracks, and then normal stresses will act across the crack faces, and frictional forces will act along the faces to resist sliding.
Aki, K. & P. G. Richards 1980. Quantitative seismology. 2 volumes. 932pp. San Francisco: Freeman. Andrews, D. J. 1985. Dynamic plane strain shear rupture with a slip-weakening friction law calculated by a boundary integral method. Bull. Seism. Soc. , 75, 1-22. Ashby, M. F. and S. D. Hallam 1986. The failure of brittle solids containing small cracks under compressive stress states. Acta Metall. 34, 497-510. Atkinson, B. K. 1980. Stress corrosion and the rate-dependent tensile failure of a fine-grained quartz rock.