The crystal structure of bornemanite, ideally Na 6 &BaTi 2 Nb(Si 2 O 7 ) 2 (PO 4 )O 2 (OH)F, a = 5.4587(3), b = 7.1421(5), c = 24.528(2) Å , a = 96.790(1), b = 96.927(1), g = 90.326(1)º, V = 942.4(2) Å 3 , space group P1, Z = 2, D calc. = 3.342 g cm À3 , from the Lovozero alkaline massif, Kola Peninsula, Russia, has been solved and refined to R 1 = 6.36% on the basis of 4414 unique reflections (F o >4sF). Electron microprobe analysis yielded the empirical formula (Na 6 .0 7 Mn 2 + 0 . 2 3 Ca 0 .0 6 & 0 . 6 4 ) S 7 . 0 0 . The crystal structure of bornemanite is a combination of a TS (titanium silicate) block and an I (intermediate) block. The TS block consists of HOH sheets (H-heteropolyhedral, O-octahedral). The TS block exhibits linkage and stereochemistry typical for Group III (Ti = 3 a.p.f.u.) of Ti-disilicate minerals: two H sheets connect to the O sheet such that two (Si 2 O 7 ) groups link to the trans edges of a Ti octahedron of the O sheet. The O sheet cations give Na 3 Ti (4 a.p.f.u.). The TS block has two different H sheets, H 1 and H 2 , where (Si 2 O 7 ) groups link to [5] Ti and [6] Nb polyhedra, and there are two peripheral sites which are occupied by Ba and Na, respectively. There are two I blocks: the I 1 block is a layer of Ba atoms; the I 2 block consists of Na polyhedra and (PO 4 ) tetrahedra.