“…The interaction of As and V cations in copper(II) minerals, as a rule, is determined by complementary isomorphic substitutions at the positions of tetrahedral centers of [T 5+ O 4 ] polyhedra, e.g., aleutite Cu 5 O 2 (AsO 4 )(VO 4 )·(Cu 0.5 □ 0.5 )Cl and coparsite Cu 4 O 2 [(As,V)O 4 ]Cl . The family of M 2+ (VO) 2 (TO 4 ) 2 (M = Ca, Co, Ni, Cu, Sr, Cd, Ba, Pb; T = P, As) compounds includes dozens of different representatives with rich polymorphism (Table S1): Cu(VO) 2 (PO 4 ) 2 , α,β-Ni(VO) 2 (PO 4 ) 2 , α,β-Co(VO) 2 (PO 4 ) 2 , α,β-Sr(VO) 2 (AsO 4 ) 2 , , Ba(VO) 2 (AsO 4 ) 2 , Ba(VO) 2 (PO 4 ) 2 , Ca(VO) 2 (PO 4 ) 2 , Sr(VO) 2 (PO 4 ) 2 , Cd(VO) 2 (PO 4 ) 2 , and Pb(VO) 2 (PO 4 ) 2 . Structural features of the M 2+ (VO) 2 (TO 4 ) 2 family have not been discussed to date.…”