Abstract
The experimental studies reviewed in Chapter 3 and 5 have been concerned only with brittle fracture from a macroscopic point of view; brittle fracture is viewed as a singular event, occurring after an unrelated, essentially elastic deformation and characterized by the peak stress or “fracture stress”. The theoretical approach of Chapter 4 sets out from the same viewpoint, but it is soon apparent that the brittle failure has to be seen as the culmination of a progressive development of cracking. Closer observation supports this view and has yielded a great deal of information bearing on the mechanism of brittle failure, especially under predominantly compressive conditions.
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© 1978 Springer-Verlag Berlin Heidelberg
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Paterson, M.S. (1978). Pre-Failure, Post-Failure, and Mechanistic Aspects of Brittle Behaviour. In: Experimental Rock Deformation — The Brittle Field. Minerals and Rocks, vol 13. Springer, Berlin, Heidelberg. https://doi.org/10.1007/978-3-662-11720-0_7
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DOI: https://doi.org/10.1007/978-3-662-11720-0_7
Publisher Name: Springer, Berlin, Heidelberg
Print ISBN: 978-3-662-11722-4
Online ISBN: 978-3-662-11720-0
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