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Labradorite (a variety of Anorthite)
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Discovered in 1780; IMA status: Not Valid (variety name)
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Chemistry
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Chemical
Formula: |
(Ca,Na)Al(Al,Si)Si2O8
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Calcium
Sodium Aluminum Silicate |
Molecular
Weight: |
271.81 gm
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Composition: |
Sodium |
3.38 % |
Na |
4.56 % |
Na2O |
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Calcium |
8.85 % |
Ca |
12.38 % |
CaO |
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Aluminum |
15.88 % |
Al |
30.01 % |
Al2O3 |
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Silicon |
24.80 % |
Si |
53.05 % |
SiO2 |
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Oxygen |
47.09 % |
O |
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100.00 % |
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100.00 % |
= TOTAL OXIDE |
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Classification
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Mineral
Classification: |
Silicates
(Germanates)
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Strunz 8th
Ed. ID:
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8/J.07-50
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Nickel-Strunz 10th
Ed. ID:
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9.FA.35
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9 : SILICATES (Germanates)
F : Tektosilicates without zeolitic H2O
A : Tektosilicates without additional non-tetrahedral anions
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Related
to: |
Feldspar
Group. A variety of Anorthite.
Plagioclase series. An intermediate member of the Albite-Anorthite Series.
High- and low-temperature structural varieties are recognized.
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Members
of Group: |
Feldspar
Group:
Albite,
Amazonite, Andesine, Anorthite, Anorthoclase, Banalsite,
Buddingtonite, Bytownite, Celsian, Dmisteinbergite,
Hyalophane, Labradorite, Microcline, Oligoclase, Orthoclase,
Paracelsian, Reedmergnerite, Sanidine, Slawsonite, Stronalsite,
Svyatoslavite
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Varieties: |
Lynx
Eye
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Synonyms: |
Black Moonstone,
Carnatite, Labrador Feldspar, Labrador Moonstone, Mauilite,
Opaline Feldspar, Radauite, Silicite, Spectrolite
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Crystal
Data
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Crystallography:
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Triclinic - Pinacoidal
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Crystal
Habit:
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Crystals
typically thin, tabular along [010], and rhombic in
section, to 4 cm. Cleavable, granular, or massive.
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Twinning:
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Common
according to Albite, Pericline, Carlsbad, Baveno, or
Manebach laws
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Physical
Properties
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Cleavage: |
Perfect
on {001}, less perfect on {010}, intersecting at 90º;
distinct on {110}
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Fracture: |
Irregular/uneven
to conchoidal
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Tenacity:
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Brittle
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Moh's
Hardness: |
6.0
- 6.5;
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Density:
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2.68
- 2.72 (g/cm3)
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Luminescence:
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None
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Radioactivity:
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Not
Radioactive
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Optical
Properties
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Color: |
Gray,
brown, greenish, blue, yellow, colorless; commonly exhibits
iridescence, especially on {010}; colorless in thin
section.
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Transparency: |
Translucent
to transparent |
Luster: |
Vitreous;
pearly on cleavages |
Refractive
Index: |
1.554
- 1.573 Biaxial ( + )
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Birefringence: |
0.008
- 0.010
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Dispersion: |
None to weak; r > v |
Pleochroism: |
n/a |
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Occurances
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Geological
Setting: |
In
mafic igneous rocks and anorthosites. Rarer in metamorphic
rocks, as amphibolites. As detrital grains in sedimentary
rocks. |
Common
Associations: |
Olivine,
Pyroxenes, Amphiboles, Magnetite |
Common
Impurities: |
n/a
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Type
Locality: |
Ford Harbour, Paul Island, near Nain, off the east coast of Labrador, Canada
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Year
Discovered: |
1780
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View
mineral photos: |
Labradorite
Mineral Photos and Locations |
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More
Information
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Mindat.org
Webmineral.com
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Labradorite
is a variety of Anorthite
which is a member of the plagioclase Feldspars of the Feldspar Group of minerals that includes Albite,
Amazonite,
Andesine, Anorthite, Bytownite, Hyalophane, Labradorite,
Moonstone,
Oligoclase, Orthoclase, Sanidine
and Sunstone. Although
Labradorite is considered a variety of Anorthite, it is
actually a mixture of Albite and Anorthite often with
a small percentage of Orthoclase. It is an intermediate member of the Albite-Anorthite Series.
Chemical analysis shows that Labradorite always has
an Anorithe content of 44 to 61 percent, which
in mineralogy is referred to as the ”Bøggild
Range”. Within the material, the twinned Anorithe and
Albite crystals are aligned in parallel lamellae of
varying thickness, usually according to the albite law.
Labradorite
is a member of the Plagioclase Feldspars of the Feldspar Group of minerals that also
includes Albite,
Amazonite,
Andesine, Anorthite, Bytownite, Hyalophane, Labradorite,
Moonstone,
Oligoclase, Orthoclase, Sanidine
and Sunstone. Labradorite
may be best known for the opaque variety with a color
play of iridescent colors that includes blues, greens,
gold, orange, yellow and purple. The transparent variety
ranges in color from colorless to yellow. It occassionally has
inclusions of small to microscopic particles of colloidal
copper which creates the effect of schiller. Schiller
is the reflection of light off the copper particles
suspended in the gem. This type of Labradorite with
schiller is called Sunstone.
Labradorite
was named in 1780 by German geologist Abraham Gottlob Werner (1749-1817)
for the location of its discovery in 1770 at Ford Harbour, Paul Island, Labrador, Canada.
Labradorite
distribution: widespread. From Ford Harbour,
Pauls Island, Labrador, Newfoundland; at Lake St. John,
Quebec; and elsewhere in Canada. In the USA, especially
in northern New York, forming the Adirondack Mountains;
crystals from Sagebrush Flat, about 37 km north of Plush,
Lake County, Oregon; atop the San Marcos Mountains,
San Diego County, and in the western San Gabriel Mountains,
Los Angeles County, California. Abundant gem crystals
in the Pinacate volcanic field, Sonora, Mexico. At Vesuvius,
Campania, and on Mt. Etna, Sicily, Italy. From Ylämaa,
near Lappeenranta, Finland. In the Langesundsfjord-
Larvik-Tvedalen area, Norway. On Surtsey Island, south
of Iceland.
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