Abstract
Adachiite, CaFe3Al6(Si5AlO18)(BO3)3(OH)3(OH), a Si–poor member of the tourmaline supergroup, is found in the hydrothermal vein cutting emery from Nabagasako of the Kiura mine, Saiki City, Oita Prefecture, Japan. Adachiite occurs as a constituent (several to 300 µm thickness) of hexagonal prismatic crystals, and forms a zoned structure closely associated with schorl. It is transparent with brownish–purple to bluish–purple color, while the massive aggregate shows black in color. Adachiite is trigonal, R3m, a = 15.9290(2), c = 7.1830(1) Å, V = 1578.39(4) Å3, and Z = 3, determined via single crystal XRD refinement (R1 = 0.038). Adachiite is the first member of the tourmaline group formed via Tschermak–like substitution.
