Andesine

Source: Wikipedia, the free encyclopedia.
Andesine
2V angle
Measured: 76° to 83°
Diagnostic featuresRequires optical/chemical analysis
References[1][2][3][4]

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.[2]

The plagioclase feldspars are a continuous solid solution series and as such the accurate identification of individual members requires detailed

specific gravity increase directly with calcium content.[5]

It is sometimes used as a gemstone.[6]

Name and discovery

Andesine was first described in 1841 for an occurrence in the Marmato mine, Marmato, Cauca, Chocó Department, Colombia.[3][4] The name is for the Andes due to its abundance in the andesite lavas in those mountains.[2][5]

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.[7]

Occurrence

Andesine occurs in

antiperthite texture. It also occurs as detrital grains in sedimentary rocks. It is commonly associated with quartz, potassium feldspar, biotite, hornblende, and magnetite.[2]

References

  1. ^ Mineralienatlas
  2. ^ a b c d Handbook of Mineralogy
  3. ^ a b Webmineral data
  4. ^ a b Mindat.org
  5. ^
  6. ^ Tables of Gemstone Identification By Roger Dedeyne, Ivo Quintens p.118
  7. ^ "Three Occurrences of Oregon Sunstone | Gems & Gemology".

External links