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oligoclase
[ ol-i-goh-kleys ]
noun
- a kind of plagioclase feldspar occurring commonly in white crystals, sometimes shaded with gray, green, or red.
oligoclase
/ ˈɒlɪɡəʊˌkleɪs /
noun
- a white, bluish, or reddish-yellow feldspar mineral of the plagioclase series, consisting of aluminium silicates of sodium and calcium. Formula: NaAlSi 3 O 8 .CaAl 2 Si 2 O 8
oligoclase
/ ŏl′ĭ-gō-klās′,ō′lĭ- /
- A white to gray triclinic mineral of the plagioclase feldspar group. Oligoclase occurs in igneous rocks with a relatively high silica content, such as granite. Chemical formula: (Na,Ca)(Al,Si)AlSi 2 O 8 .
Word History and Origins
Origin of oligoclase1
Word History and Origins
Origin of oligoclase1
Example Sentences
A variety of translucent quartz, spangled throughout with scales of yellow mica. ÷ feldspar, a variety of oligoclase with internal firelike reflections due to the presence of minute crystals, probably of hematite; sunstone.
Their felspar ranges from oligoclase to andesite and labradorite, and is often very zonal; sanidine occurs also in some dacites, and when abundant gives rise to rocks which form transitions to the rhyolites.
F� de Nuevo-Mexico, the Si�rra de San Francisco, west of the Rocky Mountains and Pueblo Zuni, consist of hornblende, oligoclase, and brown mica.
Felspar if present may be orthoclase and oligoclase.
These larger felspars have no crystalline outlines and consist of orthoclase or microcline surrounded by borders of white oligoclase.
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