The mechanism of deformation and rupture of stiff overconsolidated intact clays is a subject of relevant importance. With regard to this a number of researchers have recently stressed the role of strain localisation, which leads to formation of shear zones. Failure is the final result of such a process.
Mechanisms of rupture of reconstituted and natural fissured clay shales in undrained triaxial tests / Olivares, L.; Urciuoli, Gianfranco; Picarelli, L.. - STAMPA. - (1998), pp. 229-234.
Mechanisms of rupture of reconstituted and natural fissured clay shales in undrained triaxial tests
URCIUOLI, GIANFRANCO;
1998
Abstract
The mechanism of deformation and rupture of stiff overconsolidated intact clays is a subject of relevant importance. With regard to this a number of researchers have recently stressed the role of strain localisation, which leads to formation of shear zones. Failure is the final result of such a process.File in questo prodotto:
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