Detailed mapping of superposed fabrics and their mineral support allows for reconstruction of the tectonometamorphic evolution of the Ivozio Complex, within the inner portion of the Sesia-Lanzo Zone (Western Italian Alps). The resulting evolution is characterized by a multi-stage structural and metamorphic re-equilibration during Alpine subduction, starting from the pre-Alpine igneous association (Amp₀ + Cpx₀). The prograde associations begin with S_1a marked by Amp_I + Zo_I which pre-date the growth of Grt_I (S_1b); successive increase in pressure stabilizes a second generation of Amp + Grt (S_1c Amp_II + ZoI + Grt_II). The growth of prograde lawsonite and omphacite occur during S_1d (Omp_I + Lws + Grt_II + Amp_II) within lawsonite-bearing eclogites, while S_1e is associated with the break-down of lawsonite, producing the association Omp_I + Ky + Zo_II + Grt_II + Amp_II (lws-bearing eclogites); S_1d-e stages are associated with Amp_II + ZoI + Grt_II + Omp_I in eclogites. The second generation of penetrative foliation (S₂), describing the retrograde evolution, is divided into S_2a (Amp_II + GrtII + Pg + Zo_II) and S_2b (Chl + AmpIII + Pg + Ab). The comparison between the reconstructed evolution of the Ivozio Complex and P–T paths inferred in the Southern Sesia-Lanzo Zone suggests a non-uniqueness of the Sesia-Lanzo Zone continental crust, during the Alpine subduction.