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Oligoclase information


Oligoclase
Oligoclase from Chihuahua, Mexico
General
Categoryplagioclase, feldspar, tectosilicate
Formula
(repeating unit)
(Ca,Na)(Al,Si)4O8, where Ca/(Ca + Na) (% anorthite) is between 10–30%
Crystal systemTriclinic
Crystal classPinacoidal (1)
(same H-M symbol)
Identification
ColorUsually white, with shades of grey, green, or red[1]
CleavagePerfect {001}, Good {010}, Poor {110}.
FractureUneven, sub-conchoidal
Mohs scale hardness6 to 6.5
LusterVitreous
StreakWhite
Specific gravity2.64 to 2.66
Refractive indexnα = 1.533–1.543; nβ = 1.537–1.548; nγ = 1.542–1.552
Birefringence1st order

Oligoclase is a rock-forming mineral belonging to the plagioclase feldspars. In chemical composition and in its crystallographic and physical characters it is intermediate between albite (NaAlSi3O8) and anorthite (CaAl2Si2O8).[1] The albite:anorthite molar ratio of oligoclase ranges from 90:10 to 70:30.

Oligoclase is a high sodium feldspar crystallizing in the triclinic system. The Mohs hardness is 6 to 6.5 and the specific gravity is 2.64 to 2.66. The refractive indices are: nα = 1.533–1.543, nβ = 1.537–1.548, and nγ = 1.542–1.552. In color it is usually white, with shades of grey, green, or red.[1]

Oligoclase is a common mineral in the more silica-rich varieties of igneous rock and in many metamorphic rocks.

  1. ^ a b c Oligoclase One or more of the preceding sentences incorporates text from a publication now in the public domain: Spencer, Leonard James (1911). "Oligoclase". In Chisholm, Hugh (ed.). Encyclopædia Britannica. Vol. 20 (11th ed.). Cambridge University Press. p. 82.

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Oligoclase

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Oligoclase is a rock-forming mineral belonging to the plagioclase feldspars. In chemical composition and in its crystallographic and physical characters...

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Sunstone

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Sunstone is a microcline or oligoclase feldspar, which when viewed from certain directions exhibits a spangled appearance. It has been found in Southern...

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Plagioclase

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silica and related volcanics such as andesite. Oligoclase is common in granite and monzonite. The name oligoclase is derived from the Greek olígos ('small,...

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List of minerals

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Osumilite Otavite Ottrelite Otwayite Varieties that are not valid species: Oligoclase (a mixture of albite and anorthite) Onyx (a monochromatic banded variety...

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Mugearite

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(/ˈmʌɡiəraɪt/) is a type of oligoclase-bearing basalt, comprising olivine, apatite, and opaque oxides. The main feldspar in mugearite is oligoclase. Mugearite is a...

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Feldspar

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follows (with percent anorthite in parentheses): albite (0 to 10) NaAlSi3O8 oligoclase (10 to 30) (Na,Ca)(Al,Si)AlSi2O8 andesine (30 to 50) NaAlSi 3O 8 – CaAl...

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Belomorite

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murchisonite, Ceylon opal, hecatolite — a decorative variety of albite (oligoclase) of white or light gray color with a distinct iridescence effect. By composition...

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Quartz monzonite

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plagioclase is typically intermediate to sodic in composition, andesine to oligoclase. Quartz is present in significant amounts. Biotite and/or hornblende constitute...

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List of gemstones by species

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(var.) Rainbow (var.) Orthoclase Unakite Plagioclase Albite Labradorite Oligoclase Sanidine Sunstone Oregon sunstone Rainbow lattice sunstone Fergusonite...

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Spilite

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produced by hydrothermal alteration of basalt, and composed of albite or oligoclase, together with chlorite, epidote, calcite, and actinolite. Spilite is...

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Trondhjemite

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variety of tonalite in which the plagioclase is mostly in the form of oligoclase. Trondhjemites that occur in the oceanic crust or in ophiolites are usually...

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Dacite

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an element of the ground-mass. The plagioclase in dacite ranges from oligoclase to andesine and labradorite. Sanidine occurs, although in small proportions...

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Rhyolite

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sometimes are present as phenocrysts. The plagioclase is usually sodium-rich (oligoclase or andesine). Cristobalite and trydimite are sometimes present along with...

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Silicate mineral

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K)AlSi3O8 Sanidine – KAlSi3O8 Plagioclase feldspars Albite – NaAlSi3O8 Oligoclase – (Na,Ca)(Si,Al)4O8     (Na:Ca 4:1) Andesine – (Na,Ca)(Si,Al)4O8     (Na:Ca...

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Quartz diorite

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with phaneritic texture. Feldspar is present as plagioclase (typically oligoclase or andesine) with 10% or less potassium feldspar. Quartz is present at...

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Tonalite

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(coarse-grained) texture. Feldspar is present as plagioclase (typically oligoclase or andesine) with alkali feldspar making up less than 10% of the total...

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Erebus crystal

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Notes: Five Senses on Erebus Mountain, E.D. (17 March 1925). "Potash-oligoclase from Mt. Erebus, Antarctic, and anorthoclase from Mt. Kenya, East Africa"...

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List of rock types

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igneous rock – A form of tonalite where plagioclase-group feldspar is oligoclase Tuff – Rock consolidated from volcanic ash Websterite – Ultramafic and...

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Trachyte

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are common accessory minerals. The plagioclase is typically sodium-rich oligoclase. The alkali feldspar is typically also sodium-rich sanidine (anorthoclase)...

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Geochemistry

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rocks, the common feldspars are orthoclase, perthite, microcline, and oligoclase—all having much silica and alkalis. In the mafic rocks labradorite, anorthite...

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Granite

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microcline and is often perthitic. The plagioclase is typically sodium-rich oligoclase. Phenocrysts are usually alkali feldspar. Granitic rocks are classified...

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Andesite

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plagioclase in andesite varies widely in sodium content, from anorthite to oligoclase, but is typically andesine, in which anorthite makes up about 40 mol%...

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Tuff

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little or no quartz, but much sanidine or anorthoclase and sometimes oligoclase feldspar, with occasional biotite, augite, and hornblende. In weathering...

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Woolamai Granite

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granite: pink coarse-grained leucocratic; contains quartz, perthite, oligoclase, biotite and accessory apatite and zircon; veins of aplite and pegmatite...

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Mineral

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varieties between them (given in order from sodium- to calcium-rich): oligoclase, andesine, labradorite, and bytownite. Other examples of series include...

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Petrography

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biotite (sp. gr. 3.1), muscovite (sp. gr. 2.85), quartz (sp. gr. 2.65), oligoclase (sp. gr. 2.64), and orthoclase (sp. gr. 2.56), the crushed minerals float...

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Metasomatism

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2008). "Albitization of granitic rocks: The mechanism of replacement of oligoclase by albite". The Canadian Mineralogist. 46 (6): 1401–1415. doi:10.3749/canmin...

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Phenocryst

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of orthoclase are enveloped within rinds of sodic plagioclase such as oligoclase. In shallow intrusives or volcanic flows phenocrysts which formed before...

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