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Cu2S-Bi2S3

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References      Anthony ,  J.W.  ,   Bideaux ,  R.A.   &   Bladh ,  K.W...
Published: 01 April 2003
of the sulfbismuthides of Ag, Pb and Cu . Soc. Mining Geol. Japan, Spec . Issue 2 , 35 – 41 . Chang , L.L.Y. & Hoda , S.H. ( 1977 ): Phase relations in the system PbS–Cu2SBi2S3 and the stability of galenobismuthite . Am. Mineral . 62 , 346 – 350 . Chen , T.T. & Chang , L.L.Y
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References      Anthony ,  J.W.  ,   Bideaux ,  R.A.   &   Bladh ,  K.W...
Published: 01 April 2003
of the sulfbismuthides of Ag, Pb and Cu . Soc. Mining Geol. Japan, Spec . Issue 2 , 35 – 41 . Chang , L.L.Y. & Hoda , S.H. ( 1977 ): Phase relations in the system PbS–Cu2SBi2S3 and the stability of galenobismuthite . Am. Mineral . 62 , 346 – 350 . Chen , T.T. & Chang , L.L.Y
Journal Article
Published: 01 April 2003
The Canadian Mineralogist (2003) 41 (2): 441–456.
... of the sulfbismuthides of Ag, Pb and Cu . Soc. Mining Geol. Japan, Spec . Issue 2 , 35 – 41 . Chang , L.L.Y. & Hoda , S.H. ( 1977 ): Phase relations in the system PbS–Cu2SBi2S3 and the stability of galenobismuthite . Am. Mineral . 62 , 346 – 350 . Chen , T.T. & Chang , L.L.Y...
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Journal Article
Published: 01 October 2003
The Canadian Mineralogist (2003) 41 (5): 1155–1166.
... . Taylor , C.M. , Radtke , A.S. & Christ , C.L. ( 1973 ): New data on cuprobismutite . J. Res. U.S. Geol. Surv . 1 , 99 – 103 . Tomeoka , K. , Ohmasa , M. & Sadanaga , R. ( 1980 ): Crystal chemical studies on some compounds in the (Cu2S)(Bi2S3) system . Mineral...
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Journal Article
Published: 01 April 2003
The Canadian Mineralogist (2003) 41 (2): 429–440.
...–Cu2S–PbS–Bi2S3 . Econ. Geol . 83 , 405 – 418 . Cheynet , B. , Dall’Aglio , M. , Garavelli , A. , Grasso , M.F. & Vurro , F. ( 2000 ): Trace elements from fumaroles at Vulcano Island (Italy): rates of transport and a thermo-chemical model . J. Volcanol. Geotherm. Res...
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Molar Ag/(Ag + Cu) of fahlores and Bi/(Bi + Sb) of aramayoites (arm) from s...
Published: 01 December 2002
) of fahlores coexisting with pyrargyrite, sphalerite, and β-miargyrite/aramayoites with molar Bi/(Bi+Sb) ( X Bi ) of 0.15, 0.20, 0.25, 0.30 and 0.35 in the Ag2S-Cu2S-ZnS-Sb2S3-Bi2S3 system. Upper solid curve calculated from equation 4 using the thermochemical database of Sack (2000) ; dotted curves
Journal Article
Published: 01 December 2003
The Canadian Mineralogist (2003) 41 (6): 1481–1501.
... 0.03 Sb 0.03 Cd 0.09 ) ∑10.02 S 20.13 from Felbertal ( Topa et al. 2003 ). Projection along [010], a axis 17.512 Å, c axis 12.869 Å. Shaded and void circles indicate two levels of y , approximately 2 Å apart. Cu2 (green) represents a mixed Cu,Fe position. Two thin layers (grey-shaded...
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Journal Article
Published: 01 June 2000
The Canadian Mineralogist (2000) 38 (3): 611–616.
... was then calculated with only one Cu position occupied to fix the origin. The additional Cu positions that appeared in the map and that could subsequently be refined conformed to the distribution found in the Pmc 2 1 model, with positions corresponding to Cu2 and Cu3 showing practically full occupancy...
FIGURES
Journal Article
Published: 01 June 2002
The Canadian Mineralogist (2002) 40 (3): 849–869.
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Journal Article
Published: 01 June 2010
The Canadian Mineralogist (2010) 48 (3): 467–481.
... sites and tetrahedrally coordinated Cu1 and Cu2 sites; all of them are only partly occupied. In the thick slabs, with distorted octahedral bismuth sites, silver partly replaces bismuth in the centrally placed octahedra. The name honors Dr. Dan Topa (University of Salzburg), ore mineralogist...
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Journal Article
Published: 01 December 2002
Mineralogical Magazine (2002) 66 (6): 1043–1062.
...) of fahlores coexisting with pyrargyrite, sphalerite, and β-miargyrite/aramayoites with molar Bi/(Bi+Sb) ( X Bi ) of 0.15, 0.20, 0.25, 0.30 and 0.35 in the Ag2S-Cu2S-ZnS-Sb2S3-Bi2S3 system. Upper solid curve calculated from equation 4 using the thermochemical database of Sack (2000) ; dotted curves...
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Journal Article
Published: 01 May 2018
European Journal of Mineralogy (2018) 30 (3): 491–505.
... 0.873(5) 0.936(3) 0.995(15)   z 0.1735(7) 0.1789(5) 0.1871(10)   U eq 0.022(2) 0.0200(16) 0.025(4) Cu2 x 0.7582(14) 0.7516(9) 0.7540(17)   y 0.248(5) 0.168(3) 0.084(14)   z 0.6730(7) 0.6788(4) 0.6907(9)   U eq 0.020(2) 0.0212(16) 0.024(3) Sb1...
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Journal Article
Published: 01 December 2001
The Canadian Mineralogist (2001) 39 (6): 1641–1652.
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Journal Article
Published: 01 October 2001
The Canadian Mineralogist (2001) 39 (5): 1377–1382.
... & Hybler 1974 , Kohatsu & Wuensch 1976 ) in regular alternation and in a 1:1 ratio. The fully occupied Cu1 and Cu2 sites have a slightly eccentric tetrahedral coordination, typical for all aikinite–bismuthinite derivatives ( e.g., Kohatsu & Wuensch 1976 ). Adjacent to these are monocapped...
FIGURES
Journal Article
Published: 01 April 2012
The Canadian Mineralogist (2012) 50 (2): 371–386.
... appear split into Pb and Bi subsites, and the octahedral site of the “cosalite-like” fragment is a partially occupied Bi site, flanked by three-fold coordinated, partly occupied Cu1 and Cu2 sites. The tetrahedral (Cu,Fe) site is split into a triangular position and a tetrahedral position. Replacement...
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Journal Article
Published: 01 July 2000
European Journal of Mineralogy (2000) 12 (4): 899–917.
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Journal Article
Published: 01 April 2012
The Canadian Mineralogist (2012) 50 (2): 295–312.
...- Pb- S7 2.633(5) S8 2.622(5) S7 2.759(3) × 2 Cu2- S8 2.739(3) × 2 S9 2.788(4) × 2 S5 2.805(5) S7 2.264(5) S9 2.936(4) × 2 S10 2.898(1) × 2 S6 3.225(3) × 2 S6 2.307(2) × 2 S10 2.953(1) S9 3.098(6) S8 3.321(4) × 2 S4 2.879(5) S9 3.413(6) TABLE...
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Journal Article
Published: 01 February 2013
The Canadian Mineralogist (2013) 51 (1): 119–142.
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Journal Article
Published: 01 February 2006
The Canadian Mineralogist (2006) 44 (1): 189–206.
... and partly occupied Cu2 position, respectively. TABLE 3. FINAL VALUES OF COORDINATES AND FOURIER AMPLITUDES OF DISPLACIVE MODULATION FUNCTIONS For all atoms situated on pure ( i.e ., t I = 0) mirror planes, no superspace modulation exists in the x 1 – x 4 section. Modulation...
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Journal Article
Published: 01 January 2019
The Canadian Mineralogist (2019) 57 (1): 117–143.
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