the abundant amphibole in the sample was previously referred to as "richterite", but the high Mn and Fe contents indicate that the composition more appropriately falls along the hjalmarite-[ferri-ghoseite] join.
normalized to 8Si=8 gives B-site occupancy as Na = 1.32 apfu; Mn2+ = 0.47 apfu; Ca = 0.20 apfu. Fe2O3 and FeO calculated from total Fe by charge balance; H2O calculated by stoichiometry.