Cuyaite, Ca 2 Mn 3+ As 3+ 14 O 24 Cl, a new mineral with an arsenite framework from near Cuya, Camarones Valley, Chile

Cuyaite (IMA2019-126), Ca 2 Mn 3+ As 3+ 14 O 24 Cl, is a new arsenite mineral from near Cuya in the Camarones Valley, Arica Province, Chile. It is associated with anhydrite, native arsenic, arsenolite, calcite, claudetite, ferrinatrite, gajardoite-3 R , leiteite, magnesiocopiapite, phosphosiderite, pyrite, realgar and talmessite and formed from the oxidation of As-bearing primary phases and alteration by saline fluids derived from evaporating meteoric water under hyperarid conditions. Cuyaite occurs as pale brown thin needles (elongated on [010]), typically in divergent sprays and subparallel intergrowths. The streak is white. Crystals are transparent with adamantine lustre; subparallel intergrowths exhibit silky lustre. The mineral has Mohs hardness of 2½, is brittle, exhibits no cleavage and has irregular fracture. The calculated density is 4.140 g cm –3 . Cuyaite is optically biaxial (–), with α = 1.87(1), β = 1.956(calc) and γ = 1.98(1), determined in white light; 2V meas = 60(1)°; and orientation: X = b and Y ^ a = 53° in obtuse β. Electron microprobe analyses provided the empirical formula Ca 2.03 Mn 3+ 0.95 (As 3+ 13.66 Sb 3+ 0.65 ) Σ14.31 O 24 Cl 0.88 . The six strongest powder X-ray diffraction lines are [ d obs Å( I )( hkl )]: 4.73(45)(111, $\bar{1}$ 12), 3.162(100)( $\bar{3}$ 14), 3.035(28)(213), 3.004(37)(204), 2.931(90)( $\bar{2}$ 15, 312) and 2.779(28)(020). Cuyaite is monoclinic, Pn , a = 14.7231(6), b = 5.58709(19), c = 17.4185(12) Å, β = 112.451(8)°, V = 1324.23(14) Å 3 and Z = 2. In the crystal structure of cuyaite ( R 1 = 0.0369 for 2095 I > 2σ I reflections), AsO 3 pyramids share O corners to form a ‘loose’ 3D framework; Jahn–Teller distorted Mn 3+ O 6 octahedra and CaO 8 polyhedra link by edges and corners to form columns; the columns also link by edge- and corner-sharing to the AsO 3 pyramids in the framework; Cl occupies channels along [010] in the framework. The Raman spectrum is consistent with the presence of multiple As 3+ O 3 groups.