Chemistry:Anorthoclase
| Anorthoclase | |
|---|---|
 Doubly terminated anorthoclase crystal from Kinki Region, Honshu, Japan. Size: 1.3 cm × 0.9 cm × 0.7 cm (0.5 in × 0.4 in × 0.3 in) | |
| General | |
| Category | Feldspar |
| Formula (repeating unit) | (Na,K)AlSi3O8 |
| Strunz classification | 9.FA.30 |
| Crystal system | Triclinic |
| Crystal class | Pinacoidal (1) (same H–M symbol) |
| Space group | C1 |
| Unit cell | a = 8.28, b = 12.97 c = 7.15 [Å]; α = 91.05° β = 116.26°, γ = 90.15°; Z = 4 |
| Identification | |
| Color | Colorless, also white, pale creamy yellow, red, green |
| Crystal habit | Short prismatic crystals; tabular, rhombic, flattened along [010] |
| Twinning | Polysynthetic twinning produces a grid pattern on [100] |
| Cleavage | Perfect on [001], other partings |
| Fracture | Uneven |
| Tenacity | Brittle |
| Mohs scale hardness | 6 |
| |re|er}} | Vitreous to pearly on cleavage planes |
| Streak | White |
| Diaphaneity | Transparent |
| Specific gravity | 2.57–2.60 |
| Optical properties | Biaxial (−) |
| Refractive index | nα = 1.519–1.529 nβ = 1.524–1.534 nγ = 1.527–1.536 |
| Birefringence | δ = 0.008 |
| 2V angle | Measured: 34°–60° |
| References | [1][2][3] |
The mineral anorthoclase ((Na,K)AlSi3O8) is a crystalline solid solution in the alkali feldspar series, in which the sodium-aluminium silicate member exists in larger proportion. It typically consists of between 10 and 36 percent of KAlSi3O8 and between 64 and 90 percent of NaAlSi3O8.[5]
Structure and stability
Anorthoclase is an intermediate member of the high albite – sanidine alkali feldspar solid solution series. Intermediate members of this series, high albite, anorthoclase and high sodium sanidine are stable at temperatures of 600 °C (1,100 °F) and above. Below 400–600 °C (800–1,100 °F) only very limited solution exists (less than about 5% on both the low albite and microcline ends).[6] Anorthoclase and high albite exhibit triclinic symmetry, whereas sanidine and the low temperature orthoclase have monoclinic symmetry.[6] If the high temperature intermediate composition alkali feldspars are allowed to cool slowly, exsolution occurs and a perthite structure results.[6]
Occurrence
Anorthoclase occurs in high temperature sodium rich volcanic and hypabyssal (shallow intrusive) rocks. The mineral is typically found as a constituent of the fine grained matrix or as small phenocrysts which may occur as loose crystals in a weathered rock.[1]
It was first described in 1885 for an occurrence on Pantelleria Island, Trapani Province, Sicily. The name is from the Greek αν-, ορθός and κλάσις (not cleaving at right-angles), for its oblique cleavage.[1][2]
See also
References
- ↑ 1.0 1.1 1.2 "Handbook of Mineralogy". http://www.handbookofmineralogy.com/pdfs/anorthoclase.pdf.
- ↑ 2.0 2.1 "Mindat.org". http://www.mindat.org/min-248.html.
- ↑ "Webmineral data". http://webmineral.com/data/Anorthoclase.shtml.
- ↑ Warr, L.N. (2021). "IMA–CNMNC approved mineral symbols". Mineralogical Magazine 85 (3): 291–320. doi:10.1180/mgm.2021.43. Bibcode: 2021MinM...85..291W.
- ↑ Deere; Howie; Zussman. Framework Silicates. Rock Forming Minerals. 4. Wiley. pp. 2–5, Fig. 1.
- ↑ 6.0 6.1 6.2 Klein, Cornelis; Hurlbut, Cornelius S. Jr.. Handbook of Mineralogy. Wiley. pp. 446–449, Fig. 11-95. ISBN 0-471-80580-7.
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