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- W2465328037 abstract "Triaxial loading of certain rocks sometimes results in faulting without fracture in the ordinary sense, or sudden displacements. A brief discussion of the theory of brittle fracture of Griffith is given to indicate why it cannot apply to this kind of ductile faulting. Such ductile faulting can be explained by the theory of plasticity for plane strain. This theory is presented for more general yield conditions than that of von Mises, and it is assumed that the stress-strain rate relations can be derived from the yield condition by a process of differentiation. This formalism is by no means original, but..." @default.
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- W2465328037 date "1960-03-01" @default.
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- W2465328037 title "Chapter 11: Faulting as a Velocity Discontinuity in Plastic Deformation" @default.
- W2465328037 doi "https://doi.org/10.1130/mem79-p293" @default.
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