Schneider, F.; Yuan, X.; Schurr, B; Mechie, J.; Sippl, Christian; Haberland, Christian; Minaev, V.; Oimahmadov, I.; Gadoev, M.; Radjabov, N.; Abdybachaev, U.; Orunbaev, S.; Negmatullaev, S.
Exhumation of ultra-high pressure metamorphic rocks testifies that the continental crust can subduct to significant depth into the mantle despite its buoyancy. However, direct observation of ongoing subduction of continental crust is rare. The Pamir is re
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