The direct observation of a shear-induced structure indilute/semidilut
e giant micellar solutions in water is reported. At rest, the micelles
are randomly oriented and the zero-shear viscosity is concentration d
ependent and varies between 10(-3) and 10(-2) Pa s. Under shear, the s
olutions have no measurable anisotropy as long as the applied shear ra
te is less than a critical value determined from optical birefringence
and electric conductivity measurements. Above this ''critical shear r
ate'', the viscosity increases,and the solution becomes strongly aniso
tropic. However, it was found that the ''critical shear rate'' depends
strongly on the gap distance of the Couette cell, thus excluding the
possibility of a phase transition at the critical shear rate. Cryo-tra
nsmission electron microscopy is used to show shear-induced aggregatio
n of wormlike micelles. It is concluded that shear induces a phase sep
aration between a surfactant rich and a surfactant poor phase at shear
rates much lower than the critical value. Initially, the surfactant r
ich phase forms a network-like superstructure with domain sizes increa
sing with shear. A strong anisotropy due to the deformation of the net
work is observed when the domain size reaches the order of the gap siz
e of the Couette. This phenomenon was observed for a large range of co
ncentrations from far below up to several times above the overlap conc
entration phi.