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We host articles and citations in collaboration with the Canadian , American , British , Japanese , French , Russian , and Italian mineral societies.
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Mineral contains: Bismuthinite   

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Berlepsch P, Makovicky E, Balić-Žunić T (2001) Crystal chemistry of meneghinite homologues and related sulfosalts. Neues Jahrbuch für Mineralogie, Monatshefte 2001, 115-135

Beudant F S (1832) Sulfures de bismuth. Bismuthine. in Traité Élémentaire de Minéralogie, 2nd Edition, (Paris) 418-421

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Izumino Y, Nakashima K, Nagashima M (2014) Cuprobismutite group minerals (cuprobismutite, hodrušhite, kupčíkite and padĕrite), other Bi-sulfosalts and Bi-tellurides from the Obari mine, Yamagata Prefecture, Japan. Journal of Mineralogical and Petrological Sciences 109, 177-190

Kharbish S, Libowitzky E, Beran A (2009) Raman spectra of isolated and interconnected pyramidal XS3 groups (X = Sb, Bi) in stibnite, bismuthinite, kermesite, stephanite and bournonite. European Journal of Mineralogy 21, 325-333

Kupčík V, Veselá-Nováková L (1970) Zur Kristallstruktur des Bismuthinits, Bi2S3. Tschermaks Mineralogische und Petrographische Mitteilungen 14, 55-59

Kyono A, Kimata M (2004) Structural variations induced by difference of the inert pair effect in the stibnite-bismuthinite solid solution series (Sb,Bi)2S3. American Mineralogist 89, 932-940

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Lundegaard L F, Makovicky E, Boffa-Ballaran T, Balić-Žunić T (2005) Crystal structure and cation lone electron pair activity of Bi2S3 between 0 and 10 GPa. Physics and Chemistry of Minerals 32, 578-584

Ondruš P, Veselovský F, Gabašová A, Hloušek J, Šrein V, Vavrín I, Skála R, Sejkora J, Drábek M (2003) Primary minerals of the Jáchymov ore district. Journal of the Czech Geological Society 48, 19-147

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Pring A, Hyde B G (1987) Structural disorder in lindströmite: a bismuthinite - aikinite derivative. The Canadian Mineralogist 25, 393-399

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Takeuchi Y, Ozawa T (1975) The structure of Cu4Bi4S9 and its relation to the structures of covellite, CuS and bismuthinite, Bi2S3. Zeitschrift für Kristallographie 141, 217-232

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