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rucklidgeite

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Journal Article
Published: 01 March 1993
The Canadian Mineralogist (1993) 31 (1): 99–104.
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Summary plots for rucklidgeite (red circles) and poubaite (purple rhombs) in the subsystem Bi3Te4–Bi3Se4–Bi3S4. Inset (upper right) shows correlation between Pb and Bi in rucklidgeite between Bi3Te4 and PbBi2Te4. Rucklidgeite data from Rucklidge (1969), Lipovetskiy et al.(1977, 1979), Zav’yalov & Begizov (1977), Harańczyk (1978), Harris et al.(1983), Sakharova et al.(1986), Criddle & Stanley (1986, 1993), Pašava et al.(1986), Spiridonov et al.(1989), McQueen (1990), McQueen & Solberg (1990), Kase et al.(1993), Maglambayan et al.(1998), Moloshag et al.(2002). Poubaite data from Čech & Vavřín (1978, 1979), Johan et al.(1987). Unnamed Bi3(Te,S)4 of Zav’yalov et al.(1978), Kojonen et al.(1991), Spiridonov (1995) and Moloshag et al.(2002) shown as blue circles. Unnamed Bi3(Te,Se,S)4 of Shimizu et al.(1995), probably a Pb-free poubaite, is shown as green rhombs. Unnamed Bi3(Te,Se,S)4 of Yefimov et al.(1989), also probably poubaite, is shown as orange rhombs. Mineral ‘C’ of Miller (1981) is marked by a blue rhomb. An unnamed Se-phase (Johan et al. 1987) is shown with gray rhombs. Grey areas on main plot and inset (right) are compositional fields for Pb-free and Pb-bearing rucklidgeite from Larga, Romania (Cook & Ciobanu 2004).
Published: 01 August 2007
F ig . 15. Summary plots for rucklidgeite (red circles) and poubaite (purple rhombs) in the subsystem Bi 3 Te 4 –Bi 3 Se 4 –Bi 3 S 4 . Inset (upper right) shows correlation between Pb and Bi in rucklidgeite between Bi 3 Te 4 and PbBi 2 Te 4 . Rucklidgeite data from Rucklidge (1969
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(a) Composition of Bi-tellurides/tellurosulphides from Larga (tetradymite, tsumoite, tellurobismuthite, rucklidgeite), plotted in terms of Bi(+Pb)− Te− (S+Se). (b) Composition of tellurides and tellurosulphides in the Bi2Te3-Bi2Se3-Bi2S3 system demonstrating the extent of solid solution along the Bi2Te2S-Bi2Te2Se join between tetradymite, Bi2Te2S and kawazulite, ideally Bi2Te2Se. (c) Compositional variation expressed in terms of Bi-Pb-(S+Se+Te), demonstrating compositions of Pb-free rucklidgeite (vein ores) and rucklidgeite (porphyry mineralization).
Published: 01 April 2004
F ig . 6. ( a ) Composition of Bi-tellurides/tellurosulphides from Larga (tetradymite, tsumoite, tellurobismuthite, rucklidgeite), plotted in terms of Bi(+Pb)− Te− (S+Se). ( b ) Composition of tellurides and tellurosulphides in the Bi 2 Te 3 -Bi 2 Se 3 -Bi 2 S 3 system demonstrating the extent
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Fig. 6.
Published: 23 January 2015
F ig . 6. Reflected-light photomicrographs (oil immersion) of telluride and associated minerals. (a) Aggregate of gold, altaite, and rucklidgeite in pyrite. Note that the bottom left margin of the aggregate is delineated by a micro-fracture (arrow). Sample DY-892-4b/892 m. (b) Aggregate
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Photomicrographs (a–d, plane-polarized reflected light, oil immersion) and SEM image (e) of stage II tellurides, native gold, and their cross-cut relation to lingbaoite. (a) Gold, galena, and chalcopyrite in pyrite fracture. Note two small lingbaoite grains (top left) have reflection color similar to gold but are slightly darker than gold. (b) Trail of lingbaoite-bearing composite inclusions cut by a fracture filled by gold (from Jian et al. 2014). (c) Gold and rucklidgeite in pyrite fracture. (d) Aggregate of rucklidgeite + altaite + volynskite + hessite in pyrite. Note that the left margin of the aggregate is delineated by a micro-fracture (arrow). (e) Trail of lingbaoite-bearing composite inclusions cut by a fracture filled by Ag–Bi–Pb telluride minerals (modified from Jian et al. 2014). Abbreviations: Alt = altaite, Au = gold, Cp = chalcopyrite, Gn = galena, Hes = hessite, Lb = lingbaoite, Py = pyrite, Rkl = rucklidgeite, Syl = sylvanite, Vol = volynskite.
Published: 01 May 2020
reflection color similar to gold but are slightly darker than gold. ( b ) Trail of lingbaoite-bearing composite inclusions cut by a fracture filled by gold (from Jian et al. 2014 ). ( c ) Gold and rucklidgeite in pyrite fracture. ( d ) Aggregate of rucklidgeite + altaite + volynskite + hessite in pyrite
Journal Article
Published: 01 May 2020
American Mineralogist (2020) 105 (5): 745–755.
... reflection color similar to gold but are slightly darker than gold. ( b ) Trail of lingbaoite-bearing composite inclusions cut by a fracture filled by gold (from Jian et al. 2014 ). ( c ) Gold and rucklidgeite in pyrite fracture. ( d ) Aggregate of rucklidgeite + altaite + volynskite + hessite in pyrite...
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Journal Article
Published: 01 April 2004
Mineralogical Magazine (2004) 68 (2): 301–321.
...F ig . 6. ( a ) Composition of Bi-tellurides/tellurosulphides from Larga (tetradymite, tsumoite, tellurobismuthite, rucklidgeite), plotted in terms of Bi(+Pb)− Te− (S+Se). ( b ) Composition of tellurides and tellurosulphides in the Bi 2 Te 3 -Bi 2 Se 3 -Bi 2 S 3 system demonstrating the extent...
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Journal Article
Published: 01 February 1991
American Mineralogist (1991) 76 (1-2): 257–265.
... or josëite-B, there is possibly a complete solid solution series from tellurian ikunolite, Bi 4 (S,Te) 3 , to sulfurian pilsenite, Bi 4 (Te,S) 3 . The unnamed mineral of Yingchen (1986) is apparently tellurian ikunolite. Rucklidgeite, Bi 3 Te 4 , has an antipilsenite, Bi 4 Te 3 , structure type. The unnamed...
Journal Article
Published: 23 January 2015
The Canadian Mineralogist (2014) 52 (5): 883–898.
...F ig . 6. Reflected-light photomicrographs (oil immersion) of telluride and associated minerals. (a) Aggregate of gold, altaite, and rucklidgeite in pyrite. Note that the bottom left margin of the aggregate is delineated by a micro-fracture (arrow). Sample DY-892-4b/892 m. (b) Aggregate...
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Journal Article
Published: 01 May 2010
Scottish Journal of Geology (2010) 46 (1): 23–30.
... 42.72 100 TABLE 3 EPMA analyses (wt%) of representative tellurides from Tombuie, Perthshire Scotland. The analyses are recalculated to the number of Te atoms in the classic formulae (altaite, PbTe; hessite, Ag 2 Te; rucklidgeite, (BiPb) 3 Te 4 ; tetradymite, Bi 2 Te 2 S). wt% Ag Pb...
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Fig. 4.
Published: 23 January 2015
in (a). This composite inclusion consists of Phase A, sylvanite, and chalcopyrite. Sample 1050-1c/1050 m. (c) Close-up view of the rucklidgeite aggregate indicated in (a). Sample 1050-1c/1050 m. (d) The composite inclusion consisting of Phase A, galena, and chalcopyrite. Sample 1050-1a/1050 m. (e) Close-up view
Journal Article
Published: 01 March 2024
Russ. Geol. Geophys. (2024) 65 (3): 425–444.
...–pyrite–quartz, pyrite–chalcopyrite–sphalerite, quartz–boulangerite, and telluride. The telluride stage is represented by hessite, altaite, volynskite, merenskyite, melonite, and rucklidgeite. Gold-bearing mineralization formed from a fluid of medium salinity (0.9–9.2 wt.% NaCl equiv.) with a predominance...
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Journal Article
Journal: Geology
Published: 28 February 2024
Geology (2024) 52 (6): 411–416.
... of multiple mineral phases that extend down to the nanoscale and display a consistent crystallization sequence ( Figs. 1 and 2 ; Fig. S1), from early to late: chalcopyrite, tellurobismuthite–rucklidgeite–native gold, calaverite, altaite, and petzite. Chalcopyrite was the earliest phase to crystallize...
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Polymetallic inclusion assemblage in quartz (plane-polarized reflected light). Arrowed inclusions in upper image are detailed in images below. See Figure S1 (see footnote 1) for the full documentation of 10 polymetallic inclusion assemblages. Abbreviations: Alt—altaite; Au—gold; Ccp—chalcopyrite; Clv—calaverite; Ptz—petzite; Ruk—rucklidgeite; Tb—tellurobismuthite.
Published: 28 February 2024
—chalcopyrite; Clv—calaverite; Ptz—petzite; Ruk—rucklidgeite; Tb—tellurobismuthite.
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Sequential photomicrographs (plane-polarized reflected light) of three polymetallic inclusions during heating in heating-freezing cell flushed with 99 mol% Ar + 1 mol% H2. First appearance of melt is indicated (white arrow). See Figure S2 (see footnote 1) for melting behavior of 21 polymetallic inclusions. Abbreviations: Au—gold; Ccp—chalcopyrite; Clv—calaverite; Ptz—petzite; Ruk—rucklidgeite; Tb—tellurobismuthite.
Published: 28 February 2024
polymetallic inclusions. Abbreviations: Au—gold; Ccp—chalcopyrite; Clv—calaverite; Ptz—petzite; Ruk—rucklidgeite; Tb—tellurobismuthite.
Journal Article
Published: 01 August 2007
The Canadian Mineralogist (2007) 45 (4): 665–708.
...F ig . 15. Summary plots for rucklidgeite (red circles) and poubaite (purple rhombs) in the subsystem Bi 3 Te 4 –Bi 3 Se 4 –Bi 3 S 4 . Inset (upper right) shows correlation between Pb and Bi in rucklidgeite between Bi 3 Te 4 and PbBi 2 Te 4 . Rucklidgeite data from Rucklidge (1969...
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Journal Article
Published: 01 June 2007
The Canadian Mineralogist (2007) 45 (3): 417–435.
.... & Pinsker , Z.G. ( 1970 ): The crystal chemistry of semiconductors with octahedral and with mixed atomic coordination . Kristallografiya 15 , 287 – 293 (in Russ.). Kase , K. , Kusachi , I. & Kishi , S. ( 1993 ): Rucklidgeite solid-solution in the Yanahara deposit, Japan...
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Distribution of polymetallic inclusions and fluid inclusions in quartz. Photomicrographs A and B were taken under transmitted light, and C–H were taken under transmitted-reflected light; A–E were enhanced by focus stacking. (A) Polymetallic inclusions occurring along healed micro-fracture in quartz. (B and C) Polymetallic inclusions and fluid inclusions coexisting in healed micro-fractures in quartz. (D–H) Detailed view of polymetallic inclusions and coexisting fluid phases. Abbreviations: Alt—altaite; Au—gold; Clv—calaverite; Ptz—petzite; Ruk—rucklidgeite; Tb—tellurobismuthite; L—liquid; V—vapor.
Published: 28 February 2024
-fracture in quartz. (B and C) Polymetallic inclusions and fluid inclusions coexisting in healed micro-fractures in quartz. (D–H) Detailed view of polymetallic inclusions and coexisting fluid phases. Abbreviations: Alt—altaite; Au—gold; Clv—calaverite; Ptz—petzite; Ruk—rucklidgeite; Tb—tellurobismuthite; L
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Micromineralogy from the Tombuie veins. (a) Electrum grains (E) with galena (G) in fractures in a pyrite (P) (reflected light photomicropgraph). (b) Minerals in the Te-bearing assemblage (back scattered electron image) showing altaite (A), hessite (H), rucklidgeite (R) and tetradymite (T). Elemental maps showing relative Pb-contents (c) Bi (d), Te (e) and Ag (f). Red represents the highest concentrations, followed by green and blue. The red rim to the hessite in (e) represents a secondary Te enrichment and similarly the red rim in (f) is secondary silver enrichment.
Published: 01 May 2010
Fig. 2 Micromineralogy from the Tombuie veins. ( a ) Electrum grains (E) with galena (G) in fractures in a pyrite (P) (reflected light photomicropgraph). ( b ) Minerals in the Te-bearing assemblage (back scattered electron image) showing altaite (A), hessite (H), rucklidgeite (R) and tetradymite
Journal Article
Published: 15 June 2015
The Canadian Mineralogist (2014) 52 (6): 981–1006.
... formula is approximately AuTe (1.97∼2.08) . Apart from 0.4 to 0.9% Ag, no other trace element was detected. TABLE 2. REPRESENTATIVE COMPOSITIONS OF TELLUROBISMUTHITE, TETRADYMITE, ALTAITE, AND RUCKLIDGEITE Altaite Tellurobismuthite Tetradymite Rucklidgeite type Vein 1 Vein 1...
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