Potassic-ferropargasite, a new member of the amphibole group, from Kabutoichiba, Mie Prefecture, central Japan

Potassic-ferropargasite, ideally KCa2(Fe42+Al)Si6Al2O22(OH)(2), is a new member of the amphibole group occurring in a schistose calcareous hornfels from Kabutoichiba, Kameyama, Mie Prefecture, central Japan. The amphibole Occurs as black subhedral to anhedral crystals, up to about 700 pin long, associated with calcite, biotite, K-feldspar. plagioclase, scapolite, chlorite and titanite. Potassic-ferropargasite is optically biaxial negative with alpha = 1.680(2), beta = 1.690 (calc.), gamma = 1.698(2) and 2V= 80-90 degrees. The mineral is monoclinic, space group C2/m, with refined Unit-Cell parameters a = 9.937(5), b = 18.108(5), c = 5.335(4) angstrom, beta = 105.30(3)degrees, V = 926.0(9) angstrom(3), Z = 2. The three strongest lines in the X-ray powder-diffraction pattern [d in angstrom (1) hkl] are 2.72 (100) 151, 8.48 (81) I 10 and 2.61 (59) 061. Electron-microprobe gave SiO2 38.08, TiO2 1.92, Al2O3 15.12, Cr2O3 0.44, FeO 19.96, MnO 0.22, MgO 6.22, CaO 11.73, Na2O 1.57, K2O 2.74, F 0.13, Cl not detected, 0 = F + Cl -0.05, total 98.08 wt%, corresponding to (K0.54Na0.42)(Sigma 0.96)(Ca1.95Na0.05)(Sigma 2.00)(Fe2.592+Mg1.44Al0.67Ti0.22Cr0.05Mn0.03)(Sigma 5.00)(Si5.91Al2.09)(Sigma 8.00)O-22 (OH1.94F0.06)(Sigma 2.00) on the basis of O = 23, assuming OH + F + Cl = 2. The crystal structure of the clinoamphibole type was refined to an R of 6.5%.