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aguilarite

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Journal Article
Published: 01 February 2013
Mineralogical Magazine (2013) 77 (1): 21–31.
...L. Bindi; N. E. Pingitore Abstract An examination of a specimen of aguilarite from the type locality provides new data on the chemistry and structure of this mineral. The chemical formula of the crystal used for the structural study is (Ag 3.98 Cu 0.02 )(Se 0.98 S 0.84 Te 0.18 ), on the basis of 6...
FIGURES
Journal Article
Published: 01 August 1974
The Canadian Mineralogist (1974) 12 (6): 365–369.
Journal Article
Published: 01 August 1936
American Mineralogist (1936) 21 (8): 532–534.
...Robert R. Coats Abstract Examination of polished specimens of ores from the Comstock Lode has revealed the presence, hitherto unsuspected, of the silver sulpho-selenide, aguilarite. Aguilarite was not recorded by E. S. Bastin 1 in the only previous paper on the ores of the Comstock Lode. It occurs...
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The crystal structure of aguilarite projected down [100]. The horizontal direction is the c axis. The Ag and X (S, Se and Te) atoms are shown as white and black spheres, respectively. The unit cell is outlined.
Published: 01 February 2013
F ig . 1. The crystal structure of aguilarite projected down [100]. The horizontal direction is the c axis. The Ag and X (S, Se and Te) atoms are shown as white and black spheres, respectively. The unit cell is outlined.
Journal Article
Published: 01 December 2004
The Canadian Mineralogist (2004) 42 (6): 1745–1755.
... prospect, Los Llantenes District of La Rioja Province, Argentina. The new mineral species is generally associated with chrisstanleyite, particularly in intimate intergrowths, clausthalite, naumannite, tiemannite, klockmannite, berzelianite, umangite and aguilarite. Mercurian silver, native gold, and two...
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Journal Article
Published: 01 February 2003
The Canadian Mineralogist (2003) 41 (1): 185–200.
... sulfide content. The association of sulfides is the main gold carrier and is dominated by pyrite, chalcopyrite, sphalerite, ± galena (grey sulfide –quartz stage). Minor phases are silver-rich sulfides and sulfosalts, such as acanthite–aguilarite (Ag 2 S–Ag 4 SSe), polybasite–pearceite [(Ag,Cu) 16 (Sb...
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Scanning electron microscopy photomicrographs of ore minerals in the K1 vein. (A) Electrum intergrown with chalcopyrite and tennantite. Sub11UC3a. (B) Subrounded electrum grains in fine-grained, poorly crystalline molybdenite and quartz from vein stage 11. Sub1UC3N014b. (C) Electrum in chalcopyrite, intergrown with quartz and adularia. Sub1UC3N014a. (D) Electrum in chalcopyrite intergrown with quartz and chlorite (weakly bladed texture). Sub11UC3c. (E) Selenian galena veins. Sub113C (K2 vein). (F) Angular aguilarite grains. Sub1UC03N014. (G) Anhedral electrum intergrown with chalcopyrite and bornite. K113 (K2 vein). (H) Subrounded, flaky molybdenite grains. Sub1UC03N014. Abbreviations: Ad = adularia, Agl = aguilarite, Bn = bornite, Chl = chlorite, Cpy = chalcopyrite, El = electrum, Mo = molybdenite, Qtz = quartz, Se-Gal = selenian galena, Tn = tennantite.
Published: 01 January 2018
in chalcopyrite, intergrown with quartz and adularia. Sub1UC3N014a. (D) Electrum in chalcopyrite intergrown with quartz and chlorite (weakly bladed texture). Sub11UC3c. (E) Selenian galena veins. Sub113C (K2 vein). (F) Angular aguilarite grains. Sub1UC03N014. (G) Anhedral electrum intergrown with chalcopyrite
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The unit-cell volume ( Å3) plotted against the Se content (a.p.f.u.). The filled symbol represents the aguilarite crystal (this study); empty symbols are data from synthetic compounds (Pingitore et al., 1992).
Published: 01 February 2013
F ig . 2. The unit-cell volume ( Å 3 ) plotted against the Se content (a.p.f.u.). The filled symbol represents the aguilarite crystal (this study); empty symbols are data from synthetic compounds ( Pingitore et al. , 1992 ).
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Variations in S and Se contents in silver sulfoselenides from the Rogovik deposit (data of electron microprobe analysis). 1, ideal compositions of acanthite, aguilarite, and naumannite; 2, data from Kuznetsov et al. (1992); 3, results of this study.
Published: 01 December 2015
Fig. 5. Variations in S and Se contents in silver sulfoselenides from the Rogovik deposit (data of electron microprobe analysis). 1 , ideal compositions of acanthite, aguilarite, and naumannite; 2 , data from Kuznetsov et al. (1992) ; 3 , results of this study.
Journal Article
Published: 01 December 2015
Russ. Geol. Geophys. (2015) 56 (12): 1738–1748.
...Fig. 5. Variations in S and Se contents in silver sulfoselenides from the Rogovik deposit (data of electron microprobe analysis). 1 , ideal compositions of acanthite, aguilarite, and naumannite; 2 , data from Kuznetsov et al. (1992) ; 3 , results of this study. ...
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Journal Article
Journal: Economic Geology
Published: 01 January 2018
Economic Geology (2018) 113 (1): 209–236.
... in chalcopyrite, intergrown with quartz and adularia. Sub1UC3N014a. (D) Electrum in chalcopyrite intergrown with quartz and chlorite (weakly bladed texture). Sub11UC3c. (E) Selenian galena veins. Sub113C (K2 vein). (F) Angular aguilarite grains. Sub1UC03N014. (G) Anhedral electrum intergrown with chalcopyrite...
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Journal Article
Journal: Economic Geology
Published: 01 May 1998
Economic Geology (1998) 93 (3): 303–325.
... of interstratified chlorite-smectite and microcrystalline quartz alternately banded with adularia and comb-texture quartz. Gold-silver-bearing minerals include electrum, aeanthite- aguilarite, polybasite-pearceite, pyrargyrite-proustite, jalpaite, mckinstryite, hessite, an Ag-Te-Se-S mineral, and tetrahedrite.The...
Journal Article
Journal: Economic Geology
Published: 01 December 1988
Economic Geology (1988) 83 (8): 1668–1682.
..., subparallel to the other margin of the caldera and also located in caldera-fill lithologies. Silver, the dominant precious metal, occurs mainly as acanthite, silver sulfantimonides, such as freibergite, and native silver. Free gold and electrum were identified optically, and aguilarite (Ag 2 SeS...
Journal Article
Journal: Economic Geology
Published: 01 August 1985
Economic Geology (1985) 80 (5): 1415–1424.
... assemblage, the temperatures for the electrum-sphalerite-pyrite-Ag- Se Te mineral (naumannite, aguilarite, hessitc) assemblage are not in good agreement with the filling temperatures of fluid inclusions. A less than unity activity of Ag 2 S in Ag-Se-Te minerals may explain this disagreement. GeoRef...
Journal Article
Published: 01 June 2010
Mineralogical Magazine (2010) 74 (3): 463–468.
... and oil (refractive index 1.515), and the results are presented in Table 1 and Fig. 1 . The reflectance values are close to those of petzite (37.8–45.0%) and hessite (39–43.6%) in air. However, kurilite has convex reflectance curves that are similar to cervelleite (Ag 4 TeS) or aguilarite (Ag 4 SeS...
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Examples of opaque inclusions in Cordilleran gold particles. (A) Gold-sphalerite association in lode sample displaying intergrowths and inclusions (Bralorne, British Columbia); (B) galena inclusion in lode Au, Nugget Zone, Lone Star, Klondike; (C) pyrite inclusion in lode gold particle, Snowy Creek, Cassiar, British Columbia; (D) pyrrhotite inclusion, detrital grain, Coffee Creek, Yukon; (E) galena and arsenopyrite inclusions, detrital particle, Independence Creek, Yukon; (F) aguilarite (Ag4SeS) inclusion in lode gold particle from Blackdome, British Columbia; (G) inclusions of chalcocite in detrital gold particle from Bridge River, British Columbia; (H) mixed inclusion of Sb- and Te-bearing galena and Bi telluride, Revenue Creek, Yukon; (I) arsenopyrite and galena, detrital grain, Soya Creek, Moosehorn Range, Yukon.
Published: 01 March 2022
, Snowy Creek, Cassiar, British Columbia; (D) pyrrhotite inclusion, detrital grain, Coffee Creek, Yukon; (E) galena and arsenopyrite inclusions, detrital particle, Independence Creek, Yukon; (F) aguilarite (Ag 4 SeS) inclusion in lode gold particle from Blackdome, British Columbia; (G) inclusions
Journal Article
Journal: Economic Geology
Published: 01 May 2002
Economic Geology (2002) 97 (3): 561–571.
... with the international J.C.P.D.S. reference no. 33-587 of uytenbogaardtite Abbreviations: Int. = Intensity, ns = not significant, nd = not determined The main ore facies is characterized by a predominance of minerals of the acanthite (Ag 2 S)-aguilarite (Ag 4 SeS) series in the form of veinlets ( Fig. 3a...
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Journal Article
Published: 19 September 2022
Mineralogical Magazine (2023) 87 (1): 34–39.
... ordering of S and Se in them seems highly improbable. The similarity in the radii of Se 2– and S 2– anions lead to their substitution in solid solutions of many related minerals and synthetic compounds. No cases of their ordering are known to date. Aguilarite, the only mineral whose official IMA formula...
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Journal Article
Published: 01 August 2003
Mineralogical Magazine (2003) 67 (4): i–ii.
.... They include description of a new mineral, motukoreaite (1977), and several records of rare or unusual minerals (e.g. aguilarite, awaruite, baricite, bayerite and doyleite, dahlite and whitlockite, terrugite and nobleite, and uricite). Most are jointly authored with the finder who arrived with the ‘unknown...
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Journal Article
Published: 01 February 2012
The Canadian Mineralogist (2012) 50 (1): 101–109.
... in a black mudstone of Miocene age and are composed of quartz in association with minor amounts of adularia, chlorite, vermiculite, johansenite, calcite, pyrite, chalcopyrite, sphalerite, galena, hematite, electrum, and silver minerals such as aguilarite, pearcite-polybasite series minerals, pyrargyrite...
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