“…The nonlinear rheology of Laponite suspensions has also been intensively studied with emphasis on thixotropy and ageing or rejuvenation under shear [27,44,45,46,47,48,49,50,51]. A few experiments have hinted to the presence of shear localization in the vicinity of the yield stress in Laponite samples [19,52,53], which provided support for discontinuous models of the yielding transition [10,26].…”