The Sapi–Shergol lawsonite-blueschist metasediments are petrologically investigated.
They experienced cold subduction history (7–8 °C/km gradient) up to 470 °C, 19 kbar.
The presence of Fe+ 3 has a non-negligible effect on P estimates.
Simultaneous growth of Grt and Lws implies discussion on equilibrium/nonequilibrium.
Peak PT estimates are close to those of blueschist accretionary complexes worldwide.