Calciborite was found as a veinlet or a mass in crystalline limestone associated with gehlenite-spurrite skarns at the Fuka mine, Okayama Prefecture, Japan. Calciborite occurs as milky white aggregates up to 1 mm in diameter with shimazakiite, fluorite, bornite and calcite. An electron microprobe analysis of calciborite gave an empirical formula (Ca
0.999Mn
0.001Co
0.001)
Σ1.001B
1.999O
4 based on O = 4. The unit cell parameters are
a = 8.373(2),
b = 13.811(8),
c = 5.012(4) Å. The mineral is optically biaxial (-), α = 1.594(2), β = 1.654(2), γ = 1.672(2) and 2
Vcalc. = 56°. The Vickers microhardness is 177 kg mm
-2 (50 g load), and the Mohs hardness number is 3.5. The measured and calculated densities are 2.88(2) and 2.881 g cm
-3, respectively. The calciborite from the Fuka mine was probably formed by a reaction of boron-bearing fluids with limestone at a temperature between 250 and 300 °C.
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