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.
1998
008042838X
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.
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Utilizza questo identificativo per citare o creare un link a questo documento: https://hdl.handle.net/11588/491904
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