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Andesine
Silicate mineral comprising 30 to 50% anorthite and albite
Silicate mineral comprising 30 to 50% anorthite and albite
| Field | Value |
|---|---|
| name | Andesine |
| category | Tectosilicate minerals |
| group | Feldspar group |
| series | Plagioclase feldspar series |
| image | Andesine-251551.jpg |
| imagesize | 260px |
| caption | Andesine |
| formula | (Ca,Na)(Al,Si)4O8, where Ca/(Ca + Na) is between 30–50% |
| system | Triclinic |
| class | Pinacoidal () |
| (same H-M symbol) | |
| symmetry | *P* |
| unit cell | a = 8.155 Å, b = 12.9 Å, |
| c = 9.16 Å; α = 93.917°, | |
| β = 116.3333°, γ = 89.166°; Z = 8 | |
| color | White, gray, green, yellow, flesh-red |
| habit | Crystals rare, to 2 cm; commonly massive or granular |
| twinning | Common following albite, pericline, and carlsbad twin laws |
| cleavage | Perfect on {001}, good on {010} |
| fracture | Uneven to conchoidal |
| tenacity | Brittle |
| mohs | 6 – 6.5 |
| luster | Subvitreous to pearly |
| refractive | nα = 1.543 – 1.554 nβ = 1.547 – 1.559 nγ = 1.552 – 1.562 |
| opticalprop | Biaxial (+/−) |
| birefringence | δ = 0.009 |
| 2V | Measured: 76° to 83° |
| streak | White |
| gravity | 2.66 – 2.68 |
| diagnostic | Requires optical/chemical analysis |
| diaphaneity | Transparent to translucent |
| references |
(same H-M symbol) c = 9.16 Å; α = 93.917°, β = 116.3333°, γ = 89.166°; Z = 8
Andesine is a silicate mineral, a member of the plagioclase feldspar solid solution series. Its chemical formula is (Ca, Na)(Al, Si)4O8, where Ca/(Ca + Na) (% anorthite) is between 30 and 50%. The formula may be written as Na0.7-0.5Ca0.3-0.5Al1.3-1.5Si2.7-2.5O8.
The plagioclase feldspars are a continuous solid solution series and as such the accurate identification of individual members requires detailed optical study, chemical analysis or density measurements. Refractive indices and specific gravity increase directly with calcium content.
It is sometimes used as a gemstone.
Name and discovery
Andesine was first described in 1841 for an occurrence in the Marmato mine, Marmato, Cauca, Chocó Department, Colombia. The name is for the Andes due to its abundance in the andesite lavas in those mountains.
In the early 2000s, red and green gemstones began to be marketed under the name of 'andesine'. After some controversy, these gemstones were subsequently discovered to have been artificially-colored.
Occurrence
Andesine occurs in intermediate igneous rocks such as diorite, syenite, and andesite. It characteristically occurs in metamorphic rocks of granulite to amphibolite facies commonly exhibiting antiperthite texture. It also occurs as detrital grains in sedimentary rocks. It is commonly associated with quartz, potassium feldspar, biotite, hornblende, and magnetite.
Andesine controversy
In the early 2000s, a new variety of red or green gemstone resembling sunstone and called "andesine" appeared in the gem market. After much controversy and debate, most of these gemstones, allegedly sourced from China, were subsequently discovered to have been artificially colored by a copper diffusion process. A Tibetan source of bona fide (untreated) red andesine, however, was eventually verified by a number of independent groups of well-respected gemologists.
References
References
- [https://www.mineralienatlas.de/lexikon/index.php/MineralData?mineral=Andesine Mineralienatlas]
- [http://rruff.geo.arizona.edu/doclib/hom/andesine.pdf Handbook of Mineralogy]
- [http://webmineral.com/data/Andesine.shtml Webmineral data]
- [http://www.mindat.org/min-220.html Mindat.org]
- Klein, Cornelis, and Cornelius S. Hurlbut, Jr., ''Manual of Mineralogy,'' Wiley, 20th ed. 1985, p. 455 {{ISBN. 0-471-80580-7
- Tables of Gemstone Identification By Roger Dedeyne, Ivo Quintens p.118
- "Three Occurrences of Oregon Sunstone | Gems & Gemology".
- "Three occurrences of Oregon sunstone".
- Huges, Richard W.. (14 November 2011). "Tibet andesine mines; Part 2". RWH Publishing.
- Huges, Richard W.. (3 November 2010). "Tibet's andesine mines {{grey". RWH Publishing.
- Abduriyim, Ahmadjan. (10 September 2009). "A mine trip to Tibet and Inner Mongolia: Gemological study of andesine feldspar". [[Gemological Institute of America]] in Thailand (GIA Thailand).
- (2009). "The characteristics of red andesine from the Himalaya Highland, Tibet". [[The Journal of Gemmology]].
- (2008 <!--). "Visit to andesine mines in Tibet and Inner Mongolia; Gemological properties of andesine collected in Tibet and Inner Mongolia". [[Gems & Gemology]].
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