Abstract
Pomite (IMA2021-063), ideally Ca3[O37(CO3)]·37H2O, and pseudopomite (IMA2021-064), ideally Ca3.5[O37(CO3)]·32H2O, are two new polyoxometalate minerals from the Blue Streak mine, Bull Canyon, Montrose County, Colorado, U.S.A. Pomite properties: striated blades up to ~1 mm long; very dark green-blue color; green-blue streak; vitreous luster; brittle; Mohs hardness ≈2; irregular, splintery fracture; good cleavages on {010} and {001}; 2.19(2) g/cm−3 density; refractive indices in the vicinity of 1.70; weakly birefringent with little or no pleochroism. Pseudopomite properties: striated prisms and blades up to ~1 mm; very dark blue-green color; blue-green streak; vitreous luster; brittle; Mohs hardness ≈2; curved, irregular fracture; probably two fair cleavages, {100} and {001}; 2.40(2) g/cm−3 density; refractive indices in the vicinity of 1.72; no discernable birefringence or pleochroism. Electron microprobe analyses provided the empirical formulas Ca3.11[O37 (CO3)]·37H2O and Ca3.49[O37(CO3)]·29H2O for pomite and pseudopomite, respectively. Pomite is triclinic, P1, with a = 12.3668(10), b = 12.9692(12), c = 22.068(2) Å, α = 99.038(7), β = 95.689(7), γ = 103.249(7)°, V = 3368.7(5) Å3, and Z = 2. Pseudopomite is triclinic, P1, with a = 12.2910(18), b = 12.6205(15), c = 20.917(3) Å, α = 77.381(6), β = 85.965(5), γ = 64.367(7)°, V = 2853.6(7) Å3, and Z = 2. The crystal structures of both minerals (pomite, R1 = 0.103; pseudopomite, R1 = 0.116) contain a novel [O37(CO3)](1+x)– heteropolyanion, which is unique in natural and synthetic materials but has similarities to the [O36(CO3)]7– and [H8O36(CO3)]6– heteropolyanions reported in synthetic phases.