(mineralogy) A plagioclase feldspar with a composition ranging from Ab70An30 to Ab50An50, where Ab = NaAlSi3O8 and An = CaAl2Si2O8; it is a primary constituent of intermediate igneous rocks, such as andesites.
| Sci-Tech Dictionary: andesine |
(mineralogy) A plagioclase feldspar with a composition ranging from Ab70An30 to Ab50An50, where Ab = NaAlSi3O8 and An = CaAl2Si2O8; it is a primary constituent of intermediate igneous rocks, such as andesites.
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| Sci-Tech Encyclopedia: Andesine |
A plagioclase feldspar with composition Ab70An30 to Ab50An50 (Ab = NaAlSi3O8; An = CaAl2Si2O8). Andesine occurs primarily in igneous rocks, often in a glassy matrix as small, chemically zoned, lathlike crystals known as microlites. The rock types may be called andesinites (if dominantly feldspar), andesites, andesitic basalts (or olivine-bearing andesites, as in Hawaiian lava flows), or pyroxene-, hornblende- or biotite-andesites (all are volcanic). See also Andesite; Feldspar;
The symmetry of andesine is triclinic, hardness on the Mohs scale 6, specific gravity 2.69, melting point ∼1210°C (2210°F). If quenched at very high temperatures, andesine has an albitelike structure, with aluminum (Al) and silicon (Si) essentially disordered in the structural framework of the crystals. But, in the course of cooling, most natural andesines develop an Al-Si ordered structure called e-plagioclases. See also Albite; Crystal structure.
Calcic andesines and labradorites (Ab55An45-Ab40An60) may exsolve into two distinctly intergrown lamellar phases whose regularity of stacking produces beautiful interference colors like those in the feathers of a peacock. Polished specimens of this material are called spectrolite in the gem trade, and at some localities (notably eastern Finland) crystals up to 10 in. (25 cm) are mined by hand. Smaller crystals are made into cabochons for jewelry. They may be abundant enough in the host rock to be valued as a decorative stone. See also Gem; Labradorite.
| Wikipedia: Andesine |
| Andesine | |
|---|---|
Andesine |
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| General | |
| Category | plagioclase,feldspar,tectosilicate |
| Chemical formula | (Ca,Na)(Al,Si)4O8, where Ca/(Ca + Na) (% Anorthite) is between 30%-50% |
| Identification | |
| Crystal system | triclinic |
| Streak | white |
| Density | ~ 2.68 |
Andesine is a feldspar mineral, a part of the plagioclase series.
It is usually defined as having "%An" between 30 and 50.
Density is about 2.68.
See the plagioclase main article for more information.
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This entry is from Wikipedia, the leading user-contributed encyclopedia. It may not have been reviewed by professional editors (see full disclaimer)
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