1968
DOI: 10.3406/bulmi.1968.6244
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La hocartite, Ag2SnFeS4, une nouvelle espèce minérale

Abstract: Un nouveau sulfure d'argent, étain et fer a été découvert dans le minerai de Tacama (Bolivie). Sa composition chimique, obtenue à la microsonde électronique (4 analyses) correspond étroitement à la formule Ag₂SnFeS₄ et en fait l'équivalent argentifère de la stannite. Son diagramme de poudre, voisin de celui de la stannite a pu être indicé dans le système quadratique avec comme paramètres a = 5,74 et c = 10,96. Sa couleur en section polie est gris brunâtre légèrement différente de celle de la stannite et très p… Show more

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Cited by 11 publications
(8 citation statements)
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“…For Ag 2 CdSnS 4 , space group Cmc2 1 is mentioned in the literature with Ag, Cd, and Sn distributed statistically on the position 4a with (0, 0.167, 0.370) and S on another 4a position with (0, 0.176, 0.997) [20]. Similar compounds containing silver either crystallize in cubic diamond/sphalerite-related structures such as the stannite-or kesterite-type structure (such as Ag 2 Zn-SnS 4 [14], Ag 2 FeSnS 4 [13], Ag 2 ZnGeS 4 [24]) or in crystal structures derived from the hexagonal diamond/wurtzite type providing non-equivalent positions for the cations/anions (the wurtzstannite-type structure (space group Pmn2 1 ) and its derivatives with space group Pn (wurtzkesteritetype structure) or Pna2 1 ). Compounds crystallizing in the wurtzstannite-type structure are Ag 2 CdGeS 4 [4] and Ag 2 HgSnS 4 [15], whereas Ag 2 MnSnS 4 [18] and Si-bearing compounds such as Ag 2 FeSiS 4 [16] and Ag 2 ZnSiS 4 [17] crystallize in the wurtzkesterite-type structure.…”
Section: Structural Relationship Between Hexagonal Diamond and The Wurtzstannite-/wurtzkesterite-type Structurementioning
confidence: 98%
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“…For Ag 2 CdSnS 4 , space group Cmc2 1 is mentioned in the literature with Ag, Cd, and Sn distributed statistically on the position 4a with (0, 0.167, 0.370) and S on another 4a position with (0, 0.176, 0.997) [20]. Similar compounds containing silver either crystallize in cubic diamond/sphalerite-related structures such as the stannite-or kesterite-type structure (such as Ag 2 Zn-SnS 4 [14], Ag 2 FeSnS 4 [13], Ag 2 ZnGeS 4 [24]) or in crystal structures derived from the hexagonal diamond/wurtzite type providing non-equivalent positions for the cations/anions (the wurtzstannite-type structure (space group Pmn2 1 ) and its derivatives with space group Pn (wurtzkesteritetype structure) or Pna2 1 ). Compounds crystallizing in the wurtzstannite-type structure are Ag 2 CdGeS 4 [4] and Ag 2 HgSnS 4 [15], whereas Ag 2 MnSnS 4 [18] and Si-bearing compounds such as Ag 2 FeSiS 4 [16] and Ag 2 ZnSiS 4 [17] crystallize in the wurtzkesterite-type structure.…”
Section: Structural Relationship Between Hexagonal Diamond and The Wurtzstannite-/wurtzkesterite-type Structurementioning
confidence: 98%
“…Ag-containing compounds are more difficult to synthesize and less stable. Nevertheless, a few A 2 I B II C IV X 4 phases with A = Ag are known so far [4,[13][14][15][16][17][18][19]. For most Ag compounds, a stannite-or wurtzstannite-/wurtzkesterite-type structure has been presented in the literature.…”
Section: Introductionmentioning
confidence: 99%
“…Quaternary sulfides or selenides of the formula A2+IB+IIC+IVX4-II usually contain three different metals. A great variety of (semi)metals can be implemented for example A =Li, Na, Ag, Cu; B =Mn, Fe, Co, Ni, Zn, Cd; and C =Si, Ge, Sn . Many members of this class of materials crystallize in the stannite structure type named after the mineral stannite with the formula Cu 2 FeSnS 4 .…”
Section: Introductionmentioning
confidence: 99%
“…However, it has been more recently reported, with no structural details [38], that Furthermore, Ag 2 MnSnS 4 is one of the three sulfide minerals containing silver and tin found in nature. They are the hocartite, Ag 2 FeSnS 4 , found in Bolivia in 1967 [39], the pirquitasite, Ag 2 ZnSnS 4 , found in Argentina in 1980 [40], and the agmantinite, Ag 2 MnSnS 4 , found in Perú in 2014 [41], whose name has been recently approved by the Commission on New Minerals, Nomenclature and Classification of the International Mineralogical Association [41].…”
Section: Introductionmentioning
confidence: 99%