Aguilarite
| Aguilarite | |
|---|---|
 Aguilarite – San Carlos Mine, La Luz, Guanajuato municipality, Mexico. Specimen height is 3.9 cm. | |
| General | |
| Category | Sulfosalt minerals |
| Formula (repeating unit) | Ag4SeS |
| IMA symbol | Agu[1] |
| Strunz classification | 2.BA.55 |
| Dana classification | 2.4.1.3 |
| Crystal system | Monoclinic |
| Crystal class | Prismatic (2/m) (same H-M symbol)[2] |
| Space group | P21/n[2] |
| Unit cell | a = 4.2478(2), b =6.9432(3) c = 8.0042(5) [Å] β = 100.103(2)° Z = 4[2] |
| Identification | |
| Color | Bright lead-gray on fresh surfaces; dull iron-black on exposure to air. |
| Cleavage | None observed |
| Fracture | Hackly |
| Tenacity | Sectile |
| Mohs scale hardness | 2.5[3] 1–1.5[2] |
| Luster | Metallic |
| Streak | Gray-black |
| Diaphaneity | Opaque |
| Ultraviolet fluorescence | Non-fluorescent[4] |
| References | [3] |
Aguilarite is an uncommon sulfosalt mineral with formula Ag4SeS. It was described in 1891 and named for discoverer Ponciano Aguilar.
Description[edit]
Aguilarite is bright lead-gray on fresh surfaces but becomes dull iron black when exposed to air.[3] The mineral occurs with massive habit, as elongated pseudododecahedral crystals up to 3 cm (1.2 in), or as intergrowths with acanthite or naumannite.[5]
Discovery[edit]
In the late 19th century, Ponciano Aguilar, superintendent of the San Carlos mine in Guanajuato, Mexico, found several specimens of a mineral thought to be naumannite.[5][6] The samples were given to F. A. Genth for identification, who, along with S. L. Penfield, discovered that it was a new mineral. The mineral was described in the American Journal of Science in 1891 and named aguilarite in honor of Ponciano Aguilar.[6] When the International Mineralogical Association was founded, aguilarite was grandfathered as a valid mineral species.[7]
Occurrence[edit]
Aguilarite is uncommon, and forms at relatively low temperatures in hydrothermal deposits rich in silver and selenium but deficient in sulfur.[5] The mineral is known from a number of countries in North and South America, Europe, Asia, and Australasia.[3][5] Aguilarite occurs in association with acanthite, calcite, naumannite, pearceite, proustite, silver, stephanite, and quartz.[5]
Chemistry and structure[edit]
In 2013, aguilarite's chemistry and crystal structure were reexamined by Bindi and Pingitore.[2] The significant reevaluation of aguilarite did not discredit its status as a valid mineral, but it was established as the selenium analogue of acanthite instead of sulfur-rich naumannite.[8] The sample primarily studied came from the Gem and Mineral Collection of the Department of Geosciences at Princeton University.[9]
The work of Petruk et al. in 1974 formed the basis of knowledge regarding the silver–sulfur–selenium system for about forty years. They indexed their x-ray diffraction patterns of aguilarite on an orthorhombic cell similar to naumannite.[10] Bindi and Pingitore determined that aguilarite is, in fact, monoclinic and is isostructural to acanthite and not naumannite.[2] Bindi and Pingitore believe that Petruk et al. were unable to resolve closely spaced peaks due to low resolution equipment, making aguilarite appear similar to naumannite. Additionally, a number of inconsistencies in unit cell dimensions in the 1974 work show that aguilarite does not have the same structure as naumannite.[11]
The crystal structure of aguilarite consists of planes nearly parallel to (010) composed of tetrahedrally coordinated nonmetal atoms and AgX3 triangles (where X is a nonmetal). The planes are joined by twofold-coordinated silver atoms.[12]
Aguilarite is part of the acanthite-like solid solution series Ag2S–Ag2S0.4Se0.6. The mineral comprises the range from 50 atomic percent selenium up to the transition from monoclinic to orthorhombic.[8]
See also[edit]
References[edit]
- ^ Warr, L.N. (2021). "IMA–CNMNC approved mineral symbols". Mineralogical Magazine. 85 (3): 291–320. Bibcode:2021MinM...85..291W. doi:10.1180/mgm.2021.43. S2CID 235729616.
- ^ a b c d e f Bindi & Pingitore 2013, p. 21.
- ^ a b c d "Aguilarite". Mindat. Retrieved January 20, 2013.
- ^ "Aguilarite". Webmineral. Retrieved March 11, 2013.
- ^ a b c d e Anthony, John W.; Bideaux, Richard A.; Bladh, Kenneth W.; Nichols, Monte C. (eds.). "Aguilarite" (PDF). Handbook of Mineralogy. Chantilly, VA: Mineralogical Society of America.
- ^ a b Genth 1891, p. 401.
- ^ "The New IMA List of Minerals – A Work in Progress – Update: November 2012" (PDF). Commission on New Minerals, Nomenclature and Classification. International Mineralogical Association. p. 3. Archived from the original (PDF) on September 21, 2013. Retrieved January 20, 2013.
- ^ a b Bindi & Pingitore 2013, p. 30.
- ^ Bindi & Pingitore 2013, p. 23.
- ^ Bindi & Pingitore 2013, p. 22.
- ^ Bindi & Pingitore 2013, p. 29.
- ^ Bindi & Pingitore 2013, p. 26.
- Bibliography
- Bindi, L.; Pingitore, N. E. (February 2013). "On the symmetry and crystal structure of aguilarite, Ag4SeS". Mineralogical Magazine. 77 (1): 21–31. Bibcode:2013MinM...77...21B. doi:10.1180/minmag.2013.077.1.03. S2CID 101415447. (subscription required)
- Genth, F. A. (1891). Dana, James D.; Dana, Edward S. (eds.). "Aguilarite, a new species". American Journal of Science. 141 (241–246).
Further reading[edit]
- Petruk, W.; Owens, D. R.; Stewart, J. M.; Murray, E. J. (August 1974). "Observations on acanthite, aguilarite and naumannite" (PDF). The Canadian Mineralogist. 12 (6): 365–369.
External links[edit]
Media related to Aguilarite at Wikimedia Commons