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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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书目名称Deformation Processes in Minerals, Ceramics and Rocks
编辑David J. Barber,Philip G. Meredith
视频video
丛书名称The Mineralogical Society Series
图书封面Titlebook: Deformation Processes in Minerals, Ceramics and Rocks;  David J. Barber,Philip G. Meredith Book 1990 D. J. Barber, P. G. Meredith & contrib
描述This monograph has its origins in a two-day meeting with the same title held in London, England in the spring of 1987. The idea for the meeting came from members of the UK Mineral and Rock Physics Group. It was held under the auspices of, and made possible by the generous support of, the Mineralogical Society of Great Britain and Ireland. Additional financial assistance was provided by ECC International pIc and the Cookson Group pIc. The aims of the London meeting were to survey the current state of knowledge about deformation processes in non-metallic materials and to bring together both experts and less experienced Earth scientists and ceramicists who normally had little contact but shared common interests in deformation mechanisms. This monograph has similar aims and, indeed, most of its authors were keynote speakers at the meeting. Consequently, most of the contributions contain a review element in addition to the presentation and discussion of new results. In adopting this format, the editors hope that the monograph will provide a valuable state-of-the-art sourcebook, both to active researchers and also to graduate students just starting in the relevant fields.
出版日期Book 1990
关键词ceramics; formation; mineral; mineral resources
版次1
doihttps://doi.org/10.1007/978-94-011-6827-4
isbn_softcover978-94-011-6829-8
isbn_ebook978-94-011-6827-4
copyrightD. J. Barber, P. G. Meredith & contributors 1990
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Single-crack behaviour and crack statistics,f cracks, not necessarily isotropic and homogeneous, more or less interacting, so that the physical properties are those of a complex structure. In such a situation, understanding of the behaviour of a single crack may appear to be irrelevant. It should be looked at rather as a necessary, although n
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Fracture of polycrystalline ceramics, critical flaw dimensions increase in size from a scale less than characteristic micro-structure dimensions to a size which encompasses many grain diameters, the resistance to fracture increases, in certain polycrystals, by a factor of 5–10. This increase represents the difference between the fractu
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Compressive brittle fracture and the construction of multi-axial failure maps,these cracks extend to the sample surface, or if they interact with each other so that they grow in an unstable manner, then a macroscopic failure may follow. The initiation and growth of cracks from pores has been considered by Sammis & Ashby (1986): that from small angled cracks is analysed by Nem
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Brittle-to-ductile transitions in polycrystalline non-metallic materials,teristic strength and brittle or ductile deformation behaviour of crystalline solids is determined by the nature of their atomic bonding and crystal structure. Thus Frost & Ashby (1982) have recognized 21 isomechanical groups in their study of deformation mechanism maps to represent the plasticity a
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