U–Pb zircon analyses date the timing of sole metamorphism in the Semail ophiolite.
Metamorphism was diachronous at the two studied localities and spanned ≥1.3 Ma.
Early sole metamorphism was synchronous with formation of the ophiolite crust.
The data are consistent with ophiolite formation in a supra-subduction zone setting.
New models for the formation and evolution of the metamorphic sole are proposed.