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PbS-Sb2S3-Bi2S3

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Journal Article
Published: 01 April 2003
The Canadian Mineralogist (2003) 41 (2): 441–456.
..., Siberian Div., Inst. Geol. Geophys., Novosibirsk , 29 – 41 (in Russ.). Goodell , P.C. ( 1975 ): Binary and ternary sulphosalt assemblages in the Cu2S–Ag2S–PbS–As2S3–Sb2S3Bi2S3 system . Can. Mineral . 13 , 27 – 42 . Hillebrand , W.F. ( 1884 ): On an interesting variety...
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References      Anthony ,  J.W.  ,   Bideaux ,  R.A.   &   Bladh ,  K.W...
Published: 01 April 2003
(in Russ.). Goodell , P.C. ( 1975 ): Binary and ternary sulphosalt assemblages in the Cu2S–Ag2S–PbS–As2S3–Sb2S3Bi2S3 system . Can. Mineral . 13 , 27 – 42 . Hillebrand , W.F. ( 1884 ): On an interesting variety of löllingite and other minerals . Am. J. Sci . 127 , 349 – 358
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References      Anthony ,  J.W.  ,   Bideaux ,  R.A.   &   Bladh ,  K.W...
Published: 01 April 2003
(in Russ.). Goodell , P.C. ( 1975 ): Binary and ternary sulphosalt assemblages in the Cu2S–Ag2S–PbS–As2S3–Sb2S3Bi2S3 system . Can. Mineral . 13 , 27 – 42 . Hillebrand , W.F. ( 1884 ): On an interesting variety of löllingite and other minerals . Am. J. Sci . 127 , 349 – 358
Journal Article
Published: 01 February 2000
The Canadian Mineralogist (2000) 38 (1): 11–22.
... zinc–lead district . Econ. Geol . 63 , 655 – 670 . Hoda , S.N. & Chang , L.L.Y. ( 1975 ): Phase relations in the systems PbS–Ag2S–Sb2S3 and PbS–Ag2S–Bi2S3 . Am. Mineral . 60 , 621 – 633 . Hook , H.J.V. ( 1960 ): The ternary system Ag2S–Bi2S3PbS . Econ. Geol . 55...
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Journal Article
Published: 01 April 2012
The Canadian Mineralogist (2012) 50 (2): 201–218.
... Bi2S3 + K PbS )/3, a value of 41.7 GPa is obtained, which is very close to the observed one. In order to test the same relationship for berthierite, a similar equation can be written: K FeSb2S4 = (2 K Sb2S3 + K FeS )/3. In this case, the resulting value is 45.3 GPa, significantly different...
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Journal Article
Published: 01 June 2002
The Canadian Mineralogist (2002) 40 (3): 849–869.
... Pb x Bi 2− x S 3 (0 ≤ x ≤ 1), seemed to be complete following the classical works of Ohmasa & Nowacki (1970a , b) , Kohatsu & Wuensch (1971 , 1976) , Syneček & Hybler (1974) , Mumme (1975) , Horiuchi & Wuensch (1976 , 1977) , Mumme & Watts (1976) , Mumme et al...
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Journal Article
Published: 01 December 2002
Mineralogical Magazine (2002) 66 (6): 1043–1062.
... 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 calculated by scaling the activities of AgSbS 2 in equation 4 according to the ratio...
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Journal Article
Published: 01 June 2001
The Canadian Mineralogist (2001) 39 (3): 855–872.
... 3 . Pb, with concentrations in the range of 3.01–4.56 wt.%, constitutes an essential component of laitakarite. The amount of Pb incorporation is approximately constant over the entire compositional range. Construction of balanced reactions for the principal types of decomposition textures...
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Journal Article
Published: 01 December 2001
The Canadian Mineralogist (2001) 39 (6): 1641–1652.
... be chemically described as Cu 2 Ag x Pb 6−2 x Bi 8+ x (S,Se) 19 , with a wide range of substitution of Bi + Ag for 2Pb, with x ranging from 0.64 to 1.03 (probably up to 1.33), suggesting the presence of a solid-solution series in felbertalite. The measured unit-cell parameters of a felbertalite grain...
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Journal Article
Published: 01 April 2012
The Canadian Mineralogist (2012) 50 (2): 219–233.
...Ronny Kaden; Gerald Wagner; Klaus Bente Abstract Experimental results are presented concerning the synthesis, crystal chemistry and electrical characterization of Pb–Sb–S sulfosalts, especially boulangerite, Pb 5 Sb 4 S 11 . The crystals were grown by sublimation or chemical vapor transport using...
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Journal Article
Published: 01 April 2009
European Journal of Mineralogy (2009) 21 (2): 325–333.
... with a Link EDX unit. Cobalt was used for internal gain calibration. An acceleration voltage of 20 keV was applied, the channel width was set to 20 eV, matrix absorption and fluorescence effects were corrected by the ZAF-4 algorithm (Link analytical). Pyrite (S), arsenopyrite (As), galena (Pb) and native Cu...
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Journal Article
Published: 01 December 2013
The Canadian Mineralogist (2013) 51 (6): 841–850.
... experimental charges, explaining many features previously documented in metamorphosed ores. The experiments we have undertaken here attempt to (1) quantify processes that fractionate sulfide melts, (2) assess the importance of liquid immiscibility, and (3) provide a liquid line of descent in Pb- and Zn- rich...
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Journal Article
Published: 01 January 2019
The Canadian Mineralogist (2019) 57 (1): 117–143.
..., is compositionally zoned with cores overgrown by at least four concentric growth bands. Analyses of three of these showed relative enrichments in Ag, As, Au, Cu, Co, Ni, Sb, Pb, and Bi that can be grouped as follows: (1) As-Cu; (2) Ag-Sb-Pb; and (3) Au-Co-Ni(-Bi). Euhedral growth zones in pyrite with relatively low...
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Journal Article
Journal: Economic Geology
Published: 01 September 2004
Economic Geology (2004) 99 (6): 1063–1084.
..., 2002 ; Muir, 2003 ). Davis and Lin (2003) have bracketed the age of mineralization between 2685 ± 4 Ma and 2677 ± 1 Ma. More than 50 ore minerals at Hemlo fit into four general categories ( Harris, 1989 ; Table 1 ): (1) common sulfides and sulfosalts, (2) Tl-Pb-Cu-Hg-Ag–bearing sulfosalts...
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Journal Article
Published: 01 October 2010
The Canadian Mineralogist (2010) 48 (5): 1119–1126.
... along the b axis (4.13 Å). A unit cell is shown. In the order of decreasing size, circles represent S, Pb (blue), Sb (red) and Cu (green) sites. Light and dark spheres represent atoms at two y levels, ~2 Å apart. The meneghinite modules are shaded. TABLE 7. MEMBERS OF MENEGHINITE...
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Journal Article
Published: 01 October 2008
American Mineralogist (2008) 93 (10): 1630–1640.
...Nathan I. Chutas; Victor C. Kress; Mark S. Ghiorso; Richard O. Sack Abstract Significant quantities of silver can be accommodated in galena as a coupled substitution with Ag + Sb and/or Ag + Bi for 2 Pb atoms. The limitations of this solubility are quantified experimentally for the cubic ( Fm 3̅ m...
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Journal Article
Published: 01 March 2019
American Mineralogist (2019) 104 (3): 459–462.
...Wei Li; Cristiana L. Ciobanu; Ashley Slattery; Nigel J. Cook; Wenyuan Liu; Benjamin P. Wade; Guiqing Xie Abstract High-angle annular dark-field scanning transmission electron microscopy is a powerful Z -contrast technique able to depict the structural motifs in Pb-(Bi-Sb)-sulfosalts. Using two...
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Journal Article
Published: 01 April 2005
The Canadian Mineralogist (2005) 43 (2): 703–711.
...Anna Garavelli; Nadezhda N. Mozgova; Paolo Orlandi; Elena Bonaccorsi; Daniela Pinto; Yves MoëLo; Yuri S. Borodaev Abstract Vurroite, ideally Pb 20 Sn 2 (Bi,As) 22 S 54 Cl 6, is a new mineral species from the modern Pb–Bi epithermal deposit of La Fossa crater, on Vulcano Island, Italy. It occurs...
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Journal Article
Published: 01 September 2022
American Mineralogist (2022) 107 (9): 1752–1759.
...Azzurra Zucchini; Tonci Balić-Žunić; Ines E. Collings; Michael Hanfland; Paola Comodi Abstract In this paper, high-pressure data from a synchrotron X-ray diffraction study on a lillianite (Pb 3 Bi 2 S 6 ) single crystal up to ~21 GPa are presented. A phase transition from lillianite (space group...
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Journal Article
Published: 01 June 2005
The Canadian Mineralogist (2005) 43 (3): 919–933.
...): Cu 1.34(5), Hg 1.76(9), Pb 45.08(15), Sb 31.50(14), S 20.07(11), O (struct.) 0.20, sum 99.95. The chemical formula, calculated on the basis of a cation total of 53 atoms, is Cu 2.20 Hg 0.92 Pb 22.78 Sb 27.10 S 65.53 O 1.31 ( Z = 2), giving the idealized formula Cu 2 HgPb 22 Sb 28 S 64 (O,S) 2 , which...
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