Two masses of 199kg and 57kg fell, H.Backlund, Bull. Acad. Sci. Petrograd, 1916, 10, p.1817, Geol. För. Förh. Stockholm, 1917, 39, p.105, M.H.Hey, Cat. Met., 1966, p.61. Analysis, 5.48% Ni, E.P.Henderson, Am. Miner., 1941, 26, p.546 (M.A.8-195). From the shape of the two known masses, it is concluded that a third mass remains to be found, E.L.Krinov, Meteoritika, 1946, 3, p.59 (M.A.10-174), M.H.Hey [loc. cit.]. Further analysis, 5.45% Ni, 60.5 ppm Ga, 180 ppm Ge, 24 ppm Ir, J.T.Wasson, GCA, 1969, 33, p.859. Nitrogen abundance, E.K.Gibson and C.B.Moore, GCA, 1971, 35, p.877. Hg abundance, N.A.Ozerova et al., GCA, 1973, 37, p.569. Description, V.F.Buchwald, Handbook of Iron Meteorites, Univ. of California, 1975, p.333. Ar-38, Ar-39 isotopes, A.V.Fisenko et al., Meteoritika, 1979, 38, p.59. Study of phosphide morphology, A.J.Easton and H.A.Buckley, Meteoritics, 1979, 14, p.143. Re-Os isotopic composition, T.Hirata and A.Masuda, Meteoritics, 1992, 27, p.569. Cosmogenic Kr and Xe data, B.Lavielle and E.Gilabert, MAPS, 1997, 32, p.A77 (abs.). Ion probe analysis of PGEs in individual phases, W.Hsu et al., GCA, 2000, 64, p.1133.