The crystal structure of sibirskite (CaHBO 3 ) was solved by the Monte Carlo simulation using powder X -ray diffraction data and confirmed by the Rietveld refinement. The mineral sibirskite is monoclinic with space group P2 1 /a and cell constants of a = 8.643(6), b = 9.523(2), c = 3.567(3) Å, and β = 119.23(3)°. The unit cell consists of independent atoms such as calcium, boron, hydrogen, and three oxygen atoms. The calcium atom is surrounded by six oxygen atoms in an octahedral coordination, and a symmetrical pair of edge -shared CaO 6 octahedra forming a double chain elongates the crystallographic c axis. The CaO 6 double chains are not directly connected to each other. The BO 3 triangles are linked to one vertical and two shared oxygen atoms in three CaO 6 double chains to form the sibirskite structure. Sibirskite is isostructural with nahcolite (NaHCO 3 ), which consists of NaO 6 double chains and CO 3 triangles.