“…1.2, we first reduce to the case when ι p (Λ ⊗ Z p ) = H 2 ét (X, Z p ) and (ι p ) K sends the slope 1 part, i.e., D(D * ), isomorphically onto itself. By Lubin-Tate theory, for some finite flat extension V of W , there exists a lift G V of Br X to V such that h lifts to End(G V )[1/p] ( [52,Lem. 4.8]).…”