labradorite

(lăb`rədôrīt', lăbrədôr`īt), a variety of plagioclase feldsparfeldspar
or felspar
, an abundant group of rock-forming minerals which constitute 60% of the earth's crust. Chemically the feldspars are silicates of aluminum, containing sodium, potassium, iron, calcium, or barium or combinations of these elements.
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Labradorite

(named for a deposit on Labrador), a mineral of the soda-lime feldspars—the plagioclases. It is an isomorphic mixture of soda feldspar (albite) with lime feldspar (anorthite). The mineral contains 50–70 percent anorthite. It crystallizes in the triclinic system; it is colorless, white, or gray and forms complex twins, often with an attractive blue-green and golden iridescence. Its hardness is 6 on the Mohs’ scale and its density is 2,680–2,720 kg/m³. Labradorite enters into the composition of many basic magmatic rocks, including gabbros, basalts, and diabases. Rocks consisting almost entirely of labradorite are called labradoritites.

labradorite

[′lab·rə‚dȯ‚rīt]

(mineralogy)

A gray, blue, green, or brown plagioclase feldspar with composition ranging from Ab₅₀ An₅₀ to Ab₃₀ An₇₀, where Ab = NaAlSi₃O₈ and An = CaAl₂Si₂O₈; in the course of formation when the natural material cools, the feldspar sometimes exhibits a variously colored luster. Also known as Labrador spar.

References in periodicals archive ?

Hellmann R, Penisson JM, Hervig RL, Thomassin JH, Abrioux MF (2003) An EFTEM/HRTEM high-resolution study of the near surface of labradorite feldspar altered at acid pH: evidence for interfacial dissolution-reprecipitation.

Review and outlook for agromineral research in agriculture and climate mitigation

Name 1 Carbuncle 2 K feldspar 3 Albite 4 Tektite 5 Magnetite 6 Demantoid 7 Oolitic hematite 8 Pink pyroxene 9 Idocrase 10 Black hematite 11 Biotite 12 Hornblende 13 Calcite 14 Labradorite 15 Magnesite 16 Rhodonite 17 Reniform hematite 18 Banded siliceous rocks 19 Diopside 20 Selenite 21 Alabaster 22 Anhydrite 23 Moonstone 24 Barite 25 Hypersthene Table 2: Emission lines for classification based on major elements from geological samples.

Classification of Geological Samples Based on Soft Independent Modeling of Class Analogy Using Laser-Induced Breakdown Spectroscopy

Because of the anorthite content (An 61%), this plagioclase is classified as Labradorite. All spectra show an oxygen peak at approximately 0.3 KeV (Figs.

Characterization of the ashes from the 2014-2015 Turrialba volcano eruptions by means of scanning electron microscopy and energy dispersive X-Ray Spectroscopy/Caracterizacion de las cenizas de las erupciones del volcan Turrialba en 2014 y 2015 por medio de microscopia electronica de barrido y espectroscopia de rayos-x por energia dispersiva

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The matrix has a poikiloophitic texture formed predominantly by plagioclase (labradorite, [An.sub.60-65], in some grains bytownite, [An.sub.70-75]) enclosed by elongated hypidiomorphic brownish augite crystals of 0.3-0.8 mm length and isometric grains of subordinated olivine and biotite; accessory phases are apatite and magnetite.

Geochemistry and [sup.40]Ar/[sup.39]Ar age of early carboniferous dolerite sills in the southern Baltic sea/Laanemere lounaosa Vara-Karboni doleriitsete sillide geokeemia ja [sup.40]Ar/[sup.39]Ar isotoopvanus

Intaglio talisman necklace, $360; Bangles with semi precious stones, $602 each; Yellow sterling silver pearl necklace wtih labradorite beads and round zircons, $259

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Plagioclase phenocrysts (bytownite or labradorite; [An.sub.64-72]) have rims that are both similar to, and more sodic than, the calcic cores, with some solid solution variation within the cluster.

The Christmas Cove Dyke of coastal Maine, USA, and regional sources for Early Mesozoic flood basalts in northeastern North America

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On the other hand, feldspar from the central facies is classified as plagioclase, with compositions ranging from labradorite to anorthoclase ([An.sub.64-14] [Ab.sub.34-73] [Or.sub.01-12]; Table 1; Fig.

The Upper Triassic alkaline magmatism in the NW Iberian Chain (Spain)/El magmatismo alcalino del Triasico Superior en el NO de la Cadena Iberica (Espana)

Plagioclases in trachyandesites are characterized by andesine to labradorite composition (37 to 65% An, Table 1).

Petrogenesis of Quaternary shoshonitic volcanism in NE Iran (Ardabil): implication for postcollisional magmatism