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skinnerite

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Journal Article
Published: 01 June 1999
Mineralogical Magazine (1999) 63 (3): 399–411.
...Daniel E. Harlov Abstract Ag-Cu exchange equilibria between alpha -miargyrite AgSbS 2 and pyrargyrite Ag 3 SbS 3 and between chalcostibite CuSbS 2 and both pyrargyrite and high-skinnerite Cu 3 SbS 3 are reported for the temperature range 150-350 degrees C. All of these features are constrained...
Journal Article
Published: 01 June 1995
The Canadian Mineralogist (1995) 33 (3): 655–663.
Journal Article
Published: 01 February 1989
American Mineralogist (1989) 74 (1-2): 236–242.
... as the phase reported as pure Sb metal by previous investigators of the Cu‐Sb‐S system. Sb metal was interpreted by these investigators to form by subsolidus breakdown of tetrahedrite or skinnerite. A textural and compositional examination of liquidus and subliquidus phase relations on the join Cu 2 S‐Sb 2 S 3...
Journal Article
Published: 01 October 1974
American Mineralogist (1974) 59 (9-10): 889–895.
...Sven karup-Møller; Emil Makovicky Abstract A new mineral. skinnerite (Cu 3 SbS 3 with minor amounts of silver), is identical with synthetic Cu 3 SbS 3 (the B'phase of Skinner, Luce, and Makovicky, 1972). A reversible phase transfoimation takes place in both materials at about l22°C.The high...
Image
Crystal structures of wittichenite (a), skinnerite (b), and Li3SbS3 (c) as seen down b. (Color online.)
Published: 03 October 2022
Figure 6. Crystal structures of wittichenite ( a ), skinnerite ( b ), and Li 3 SbS 3 ( c ) as seen down b . (Color online.)
Journal Article
Published: 11 April 2024
Mineralogical Magazine (2024) 88 (4): 392–399.
..., associated with skinnerite, chalcostibite, famatinite, tetrahedrite-(Fe) and zoned aggregates of tennantite-(Cu) to tennantite-(Fe). Tetrahedrite-(Cu) is steel-grey, with a metallic lustre. Mohs hardness is ca . 3½–4 and calculated density is 5.029 g.cm –3 . In reflected light, tetrahedrite-(Cu) is isotropic...
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Journal Article
Published: 03 October 2022
American Mineralogist (2022) 107 (10): 1901–1909.
...Figure 6. Crystal structures of wittichenite ( a ), skinnerite ( b ), and Li 3 SbS 3 ( c ) as seen down b . (Color online.) ...
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Journal Article
Published: 20 October 2020
Mineralogical Magazine (2020) 84 (6): 859–868.
... with galena and tetrahedrite, as evidenced from experimental studies in the ternary system PbS–Cu 2 S–Sb 2 S 3 (Pruseth et al ., 1997 ). Skinnerite (Cu 12 Sb 4 S 12 ), which exists in equilibrium with the Cu 2 S-rich melt has a composition very similar to that of tetrahedrite [Cu 6 (Cu 4 Cu 2 )Sb 4 S 12 S...
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Journal Article
Journal: Economic Geology
Published: 01 October 1997
Economic Geology (1997) 92 (6): 720–732.
... of phases such as chalcostibite and skinnerite can be explained by the extremely low sulfur fugacity values, beyond the Bartonian f (sub S 2 ) -T regime, that are essential for their stability. GeoRef, Copyright 2006, American Geological Institute. Abstract, Copyright, Society of Economic Geologists 1997 ...
Journal Article
Published: 01 August 1988
American Mineralogist (1988) 73 (7-8): 707–713.
... skinnerite (Cu 3 SbS 3 ) from their end-member component sulfides (Cu 2 S and Sb 2 S 3 ) were determined to be −20.2 ± 2.1 kJ·mol −1 and −24.8 ± 2.7 kJ·mol −1 , respectively. Mixtures of solid Cu 2 S and liquid Sb 2 S 3 at 895 K were studied by solid-liquid reaction calorimetry, and by dilution calorimetry...
Journal Article
Journal: Economic Geology
Published: 01 April 1977
Economic Geology (1977) 72 (2): 271–289.
...,As)S 4 ; luzonite Cu 3 (As,Sb)S 4 ; chalcostibite, Cu(Sb,As)S 2 ; high-skinnerite, Cu 3 (Sb,As)S 3 ; compound A, Cu 24 (As,Sb) 12 S 31 ; and the solid solution series tennantite-tetrahedrite, Cu (sub 12+X) (As,Sb) (sub 4+Y) S 13 . The composition volume for tennantite-tetrahedrite is complex...
Journal Article
Published: 01 February 2018
Mineralogical Magazine (2018) 82 (1): 199–209.
... and skinnerite. In reflected light, bytízite is grey with a yellowish hue and weak bireflectance. Pleochroism is weak. Anisotropy under crossed polarisers is strong ( Fig. 1 ), with grey to brownish rotation tints. Internal reflections were not observed. Reflectance percentages for the four Commision on Ore...
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Image
(a) The composition of Melt 1 and Melt 2 (filled circles) of the run G4 projected on the ternary system Cu2S–PbS–Sb2S3 at 500°C (Pruseth et al., 1997). The tetrahedrite:galena ratio of 70:30 mol.% obtained from the dotted area in Fig. 5c coincides with point E, which is collinear with galena and skinnerite. (b) Tentative tetrahedrite–galena binary phase diagram at higher $f_{{\rm S}_ 2}$, with proposed eutectic at tetrahedrite:galena = 70:30 mol.% showing Melt 2 is unlikely to be a liquidus phase.
Published: 20 October 2020
is collinear with galena and skinnerite. ( b ) Tentative tetrahedrite–galena binary phase diagram at higher $f_{{\rm S}_ 2}$ , with proposed eutectic at tetrahedrite:galena = 70:30 mol.% showing Melt 2 is unlikely to be a liquidus phase.
Image
(a) The composition of Melt 1 and Melt 2 (filled circles) of the run G4 projected on the ternary system Cu2S–PbS–Sb2S3 at 500°C (Pruseth et al., 1997). The tetrahedrite:galena ratio of 70:30 mol.% obtained from the dotted area in Fig. 5c coincides with point E, which is collinear with galena and skinnerite. (b) Tentative tetrahedrite–galena binary phase diagram at higher $f_{{\rm S}_ 2}$, with proposed eutectic at tetrahedrite:galena = 70:30 mol.% showing Melt 2 is unlikely to be a liquidus phase.
Published: 20 October 2020
is collinear with galena and skinnerite. ( b ) Tentative tetrahedrite–galena binary phase diagram at higher $f_{{\rm S}_ 2}$ , with proposed eutectic at tetrahedrite:galena = 70:30 mol.% showing Melt 2 is unlikely to be a liquidus phase.
Image
(a) The crystal structure of P212121 wittichenite Cu3BiS3 (Kocman and Nuffield 1973) in a polyhedral representation. Projection on [010]. CuS3 triangles are stippled; BiS3 coordination pyramids are ruled.(b) The crystal structure of P21/c skinnerite Cu3SbS3 (Makovicky and Balić-Žunić 1995). Projection on [010]. Triangular CuS3 coordinations are presented as stippled triangles, SbS3 coordination pyramids are ruled. (c) The crystal structure of Cu1.78Bi4.73Se8 (Makovicky et al. 2006), the third member of the pavonite homologous series. A number of statistically occupied copper positions (sites of “frozen” Cu, small grey spheres) were detected in the octahedral columns situated in the thinner structural slabs (at z = ½; c axis vertical) as well as replacing a part of Bi (larger grey circles) in the thicker slabs.
Published: 01 January 2006
Figure 40. (a) The crystal structure of P 2 1 2 1 2 1 wittichenite Cu 3 BiS 3 ( Kocman and Nuffield 1973 ) in a polyhedral representation. Projection on [010]. CuS 3 triangles are stippled; BiS 3 coordination pyramids are ruled.(b) The crystal structure of P 2 1 / c skinnerite Cu 3 SbS 3
Journal Article
Published: 01 May 2003
American Mineralogist (2003) 88 (5-6): 931–935.
.... Electron microprobe analysis gave Cu 52.36, Zn 2.39, Fe 1.78, As 16.64, Sb 0.74, S 27.01; sum 100.92 wt%, corresponding to (Cu 2.97 Zn 0.13 Fe 0.11 ) ∑3.21 (As 0.79 Sb 0.02 ) ∑0.81 S 2.98 , simplified as Cu 3 AsS 3 . An associated mineral identified as skinnerite-like occurs as irregular to oval grains, up...
Journal Article
Published: 01 November 1983
Jour. Geol. Soc. India (1983) 24 (11): 588–593.
... values for reaction (I) were plotted in the log aS2 -T space (Fig. 2) along with the sulfidation curves for tetrahedrite/skinnerite, galena, pyrrhotite! pyrite, bournonite and chalcopyrite. DISCUSSION The univariant line representing the sulfidation reaction (td + po) + gn + 82 = bnt + cpy, has a high...
Journal Article
Published: 01 November 1998
Jour. Geol. Soc. India (1998) 52 (5): 543–547.
...(St), Skinnerite (Sk), Owyheeite (Ow), Tetrahedrite (Tt), Tenantite (Tn), Thalcusite (Th), Twinnite (Tw), Ulmanite (UI), Native Bismuth (NBi), -o:Z< and Manganoan Fahlore (Mnp). 'D 'D (lO tVI. FRErBERGITE FROM POLYMETALLIC SULPHIDE DEPOSITS, RAJASTHAN 545 Fig.I. Freibergite CFr) at the margin...
Journal Article
Published: 01 February 2002
The Canadian Mineralogist (2002) 40 (1): 1–18.
... < 0.27: Skinner et al. 1972 ). Tetrahedrite breaks down at 543°C to digenite (Cu 9 S 5 ) + famatinite (Cu 3 SbS 4 ) + skinnerite (Cu 3 SbS 3 ). Skinnerite, which has a composition close to that of tetrahedrite, melts at 608°C ( Skinner et al. 1972 ). Unlike the other ternary systems described...
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Journal Article
Journal: Economic Geology
Published: 01 September 2004
Economic Geology (2004) 99 (6): 1063–1084.
... ), all common at Hemlo, compared to the other sulfosalts ( Harris, 1989 ), would have produced melt if they all existed prior to peak metamorphism. Note that the end members, tetrahedrite (Cu 12 Sb 4 S 13 ) and freibergite (Ag 12 Sb 4 S 13 ), are considered to be analogous to skinnerite (Cu 3 SbS 3 ; T m...
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