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andorite

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Journal Article
Published: 11 May 2023
Mineralogical Magazine (2023) 87 (4): 582–590.
... 1 /n and Z = 2. Holubite is a new member of the andorite branch of the lillianite homologous series with N = 4. The structure of holubite contains two Pb sites with a trigonal prismatic coordination, eight distinct octahedral sites, of which one is a mixed (Bi,Ag) site and one is a mixed (Sb,Pb...
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Journal Article
Published: 01 September 2018
European Journal of Mineralogy (2018) 30 (5): 1021–1035.
... = 4223.3(5) Å 3 , Z = 2. The crystal structure was solved and refined to R 1 = 0.067 on the basis of 9756 reflections with F o > 4σ( F o ) and 424 refined parameters. Andreadiniite is a new 4,4 L homologue belonging to the andorite sub-series of Sb-rich members within the lillianite homologous series...
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Journal Article
Published: 01 March 1994
The Canadian Mineralogist (1994) 32 (1): 185–188.
Journal Article
Published: 01 September 1965
American Mineralogist (1965) 50 (9): 1498–1500.
...Sidney A. Williams Abstract Andorite has been found in silver ores from the Taylor district near Ely, White Pine County, Nevada. The ores occur in brecciated limestones on either side of a fault zone and consist of sphalerite, galena, enargite, bournonite, tennantite, andorite and stibnite...
Journal Article
Published: 01 April 1954
American Mineralogist (1954) 39 (3-4): 161–171.
...J. D. H. Donnay; Gabrielle Donnay Abstract Most specimens of andorite are syntaxic intergrowths of two distinct species, which have also been observed separately. Rather than revive the name sundtite, we propose to call them andorite IV and andorite VI because their c translations are multiples, 4...
Journal Article
Published: 01 May 1937
American Mineralogist (1937) 22 (5): 651–666.
Journal Article
Published: 01 April 2014
Mineralogical Magazine (2014) 78 (2): 387–414.
...E. Makovicky; D. Topa Abstract The current state of the lillianite homologous series is presented, with its two branches – the lillianite branch of the predominantly Pb-Bi-Ag sulfosalts and the andorite branch of predominantly Pb-Sb-Ag sulfosalts. Both the natural and synthetic members...
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Image
A simplified diagram of the Ag-Sb-Pb-based members of the andorite branch of the lillianite homologous series. Only the line with N = 4;4 has been found. Only the crystallographically ascertained phases are indicated. ‘DT and EM’ are new, unpublished data. For references see Table 2 and text.
Published: 01 April 2014
F ig . 5. A simplified diagram of the Ag-Sb-Pb-based members of the andorite branch of the lillianite homologous series. Only the line with N = 4;4 has been found. Only the crystallographically ascertained phases are indicated. ‘DT and EM’ are new, unpublished data. For references see Table 2
Image
Twill pattern of crankshaft chains in “senandorite” (andorite VI), ideally PbAgSb3S6 (Sawada et al. 1987). The sixfold sequence of 4 Å subcells has a distinct pattern of crankshaft chains As3S7, pairs As2S4, and marginal AsS3 groups. The twill pattern is based on one crankshaft chain along one diagonal and a pair of parallel crankshaft chains along the opposite diagonal. Circles in order of decreasing size represent: S, Pb, Ag, Sb.
Published: 01 February 2003
F igure 6. Twill pattern of crankshaft chains in “senandorite” (andorite VI), ideally PbAgSb 3 S 6 ( Sawada et al. 1987 ). The sixfold sequence of 4 Å subcells has a distinct pattern of crankshaft chains As 3 S 7 , pairs As 2 S 4 , and marginal AsS 3 groups. The twill pattern is based on one
Journal Article
Published: 11 April 2023
Mineralogical Magazine (2023) 87 (2): 225–232.
... becomes uranocircite; andorite IV becomes quatrandorite; and andorite VI becomes senandorite. The Commission on New Minerals, Nomenclature and Classification of the International Mineralogical Association (IMA–CNMNC) is an international non-profit organisation that evaluates new mineral proposals...
FIGURES
Journal Article
Published: 15 May 2018
Mineralogical Magazine (2018) 82 (4): 993–1005.
..., terrywallaceite, vikingite, treasurite, eskimoite and Bi-rich andorite-group minerals) and other bismuth sulfosalts (izoklakeite, cosalite and Bi-rich jamesonite) in quartz gangue. The mineral occurs as lath shaped crystals or anhedral grains up to 80 µm × 70 µm, growing together in aggregates up to 200 µm × 150...
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Journal Article
Published: 01 December 1968
The Canadian Mineralogist (1968) 9 (4): 478–484.
...Sidney A. Williams Silver ores at Morey occur as kryptothermal fracture fillings cutting a nevadite intrusive. Gangue minerals are rhodochrosite, quartz, pyrite, and arsenopyrite. The major silver minerals are diaphorite, owyheeite, andorite, pyrargyrite, and stephanite. Jamesonite and sphalerite...
Image
Backscattered electron images. (a) Fragments of baumstarkite with dark lamellae with high As content. (b) Baumstarkite crystals (ba) with weak compositional zonation and associated with miargyrite (mi), andorite (an), a robinsonite type material (ro), and traces of pyrargyrite (py). (c) Compositionally zoned baumstarkite, with local transition to aramayoite (ar), randomly intergrown with miargyrite (mi, Bi or As rich) and pyrargyrite (py). (d) Aramayoite with weak compositional zonation, surrounded (replaced) by a myrmekitic intergrowth of diaphorite (di) and galena-matildite s.s. (ga-ma) (lower part) and an andorite (an) like phase (upper part); owyheeite (ow) occurs as needle-shaped crystals penetrating the intergrowth. Samples in a and b are from San Genaro, Huancavelica (MBB 98.36.01, 99/49a-WHP301), c is from Pirquitas (Veta-vein Potosi; WHP1716), and d is from Armonia mine, El Quevar (EQ 95/9).
Published: 01 May 2002
F igure 1. Backscattered electron images. ( a ) Fragments of baumstarkite with dark lamellae with high As content. ( b ) Baumstarkite crystals (ba) with weak compositional zonation and associated with miargyrite (mi), andorite (an), a robinsonite type material (ro), and traces of pyrargyrite
Journal Article
Published: 01 October 2009
The Canadian Mineralogist (2009) 47 (5): 1257–1264.
... ): Saint, Version 6.0. Bruker AXS Inc ., Madison, Wisconsin, USA . Hellner , E. ( 1958 ): A structural scheme for sulfide minerals . J. Geol . 66 , 503 – 525 . Kaspar , P. , Mrazek , Z. & Ridkosil , T. ( 1983 ): Andorite, fizelyite, and miargyrite: a decomposition...
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Journal Article
Published: 01 July 2011
American Mineralogist (2011) 96 (7): 1186–1189.
... 15 02 2011 © 2011 American Mineralogist 2011 Uchucchacuaite fizélyite ramdohrite andorite series sulfosalts crystal structure single-crystal X-ray diffraction Uchucchacuaite, AgMnPb 3 Sb 5 S 12 , belongs to the Sb-rich andorite subgroup in the lillianite homeotypic series...
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Journal Article
Published: 01 April 2013
American Mineralogist (2013) 98 (4): 773–779.
... that share two common S atoms via short bonds. Relationships to, and differenced from, fizelyite and uchucchacuaite are described and discussed. The andorite–fizelyite substitution series, ideally Pb 3 Sb 2 S 6 –PbAgSbS 3 , is the N = 4 subset of the more general lillianite homologous series. Its internal...
FIGURES
Journal Article
Published: 01 August 2016
Mineralogical Magazine (2016) 80 (5): 809–817.
...(31)(182). Comparison with gustavite, andorite and roshchinite confirms its independence as a mineral species. Colorada, which is the principal vein, follows a distinct fault zone for more than 1800 m along strike. Other veins which parallel the Colorada structure are Arturo and Animas towards...
FIGURES
Journal Article
Published: 01 October 2010
European Journal of Mineralogy (2010) 22 (5): 741–750.
... mine dumps of the Staročeske (Old Bohemian) Lode in the Kutná Hora vein Ag–Pb–Zn deposit, Czech Republic. The colour of granular aggregates of Bi–Sb–Pb–Ag sulphosalts is very light silvery grey, with metallic lustre and black streak. The maximum size of gustavite and andorite crystal aggregates...
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Journal Article
Published: 01 March 2014
European Journal of Mineralogy (2014) 26 (1): 163–170.
..., Hg-rich oversubstituted andorite, realgar, sphalerite, and Hg-rich tetrahedrite. Electron-microprobe data give (in wt%): Cu 4.79(7), Ag 2.00(5), Fe 0.12(1), Hg 37.31(23), Zn 0.98(1), Cd 0.11(7), Tl 19.19(16), As 9.96(31), Sb 7.16(35), S 18.86(7), Cl 0.05(1), total 100.53(18). The structural formula...
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Book Chapter

Author(s)
S. Rivas
Series: AAPG Memoir
Published: 01 January 1976
EISBN: 9781629812113
..., the lode deposits are related to small stocks and dikes of dacite and rhyolite of Pliocene age. The belt widens (100 km) and forms the famous polymetallic province, unique in the world because of the rare associations of tin, silver, and other minerals such as teallite, franckeite, aramayoite, andorite...