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Allanite-(Ce)
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Discovered in 1810; IMA status: Valid (pre-IMA; Grandfathered)
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Chemistry
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Chemical
Formula: |
(Ca;Ce)2(Al;Fe2+;Fe3+)3(SiO4)(Si2O7)O(OH)
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Calcium
Cerium Yttrium Aluminum Iron Silicate Hydroxide |
Molecular
Weight: |
614.71 gm |
Composition: |
Calcium |
3.91 % |
Ca |
5.47 % |
CaO |
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Cerium |
27.35 % |
Ce |
32.04 % |
Ce2O3 |
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Yttrium |
4.34 % |
Y |
5.51 % |
Y2O3 |
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Aluminum |
9.88 % |
Al |
18.66 % |
Al2O3 |
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Iron |
6.81 % |
Fe |
9.74 % |
Fe2O3 |
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Silicon |
13.71 % |
Si |
29.32 % |
SiO2 |
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Hydrogen |
0.16 % |
H |
1.47 % |
H2O |
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Oxygen |
33.84 % |
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/C.23-80
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Nickel-Strunz 10th
Ed. ID:
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9.BG.05
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9 : SILICATES (Germanates)
B : Sorosilicates G :
Sorosilicates with mixed SiO4 and Si2O7 groups;
cations in octahedral [6] and greater coordination
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Related
to: |
Epidote
Group
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Members
of Group: |
Epidote
Group: Allanite, Askagenite, Clinozoisite, Dissakisite,
Dollaseite, Epidote, Ferriallanite, Khristovite,
Manganiandrosite, Manganipiemontite, Mukhinite, Piemontite,
Uedaite, Vanadoandrosite, Zoisite
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Varieties: |
Chromian Allanite-(Ce),
Allanite-(Ce), Allanite-(La), Allanite-(Y)
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Synonyms: |
Cerepidote,
Cerine, Cerorthite
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Crystal
Data
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Crystallography:
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Monoclinic
- Prismatic
(may be metamict - a mineral originally crystalline, eventually amorphous due to radiation damage)
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Crystal
Habit:
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Crystals
tabular, or prismatic to acicular, to 90 cm; granular,
massive.
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Twinning:
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Polysynthetic,
common on [100]
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Physical
Properties
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Cleavage: |
Imperfect
on [001], Poor on [100], Poor on [110]
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Fracture: |
Irregular/Uneven,
Conchoidal
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Tenacity:
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Brittle
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Moh's
Hardness: |
5.5 - 6.0
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Density:
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3.50
- 4.20 (g/cm3)
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Luminescence:
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None
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Radioactivity:
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Weak;
GRapi = 27,438.55 (Gamma Ray American Petroleum Institute Units)
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Optical
Properties
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Color: |
Black,
dark Brown, dark Reddish Brown, dark Greenish Brown
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Transparency: |
Translucent
to Opaque |
Luster: |
Vitreous,
Resinous to Sub-Metallic |
Refractive
Index: |
1.715
- 1.822 Biaxial ( - ); Metamict Allanites are isotropic with N as low as 1.61
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Birefringence: |
0.018 - 0.031
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Dispersion: |
Distinct
to Strong; r > v |
Pleochroism: |
X
= pale olive-green, reddish brown; Y = dark brown,
brownish yellow; Z = dark reddish brown, greenish
brown
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Occurances
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Geological
Setting: |
An
accessory in some granites and granite pegmatites, syenites,
more rarely in gabbroic pegmatites. Rarely in schists,
gneisses, and some contact metamorphosed limestones;
a clastic component of sediments. |
Common
Associations: |
Epidote,
Fluorite, Muscovite |
Common
Impurities: |
None
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Type
Locality: |
Aluk Island, Prins Christian Sound, Kitaa (West
Greenland) Province, Greenland |
Year
Discovered: |
1810
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View
mineral photos: |
Allanite
Mineral Photos and Locations |
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Unusual Gem Categories
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Metamict Gems, Radioactive Gems
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More
Information
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Mindat.org
Webmineral.com
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Allanite-(Ce)
is
a rare member of the Epidote Group of minerals that
includes Allanite, Clinozoisite, Epidote,
Hancockite, Mukhinite,
Piedmontite, Tanzanite,
Thulite
and Zoisite. Allanite is usually opaque black but may also be found as light to dark brown or greenish brown crystals. The black, opaque crystals are usually larger and the transparent brownish crystals are usually too small for faceting.
Because Allanite is a weakly radioactive mineral it should be stored away from other gems and minerals that
are subject to damage from radioactivity and of course human exposure
should be limited.
Allanite is usually metamict due to the presence of radioactive Cerium (Ce) in its chemical composition. Metamictization is a natural, gradual process of destruction of the internal crystal structure of a mineral due to radiation present in the mineral or from nearby external radiation. Metamictization eventually leaves the mineral amorphous or without any internal crystal structure. Once this process is complete the mineral is described as metamict.
Allanite was named in 1810 by British chemist and mineralogist Thomas Thomson (1773-1852) to honor Scottish mineralogist Thomas Allan (1777-1833), who first observed the mineral.
Allanite is found at many locations worldwide. Some locations for good crystals follow. From Qáqarssuatsiaq, Alluk, south Greenland.
At Ytterby and Finbo, Sweden. From Kragerö, Arendal,
and on Hitterö Island, Flekkefjord, Norway. From Sillböle,
Stansvik, and Vaarala, Finland. At Miass, Ilmen Mountains,
Southern Ural Mountains, Russia. From the Trimouns talc
deposit, six km northeast of Luzenac, Ariμege, France.
In the USA, at Pacoima Canyon, Los Angeles County, California;
in the Baringer Hill pegmatite, 26 km west of Burnet,
and on the Rode Ranch, Llano County, Texas. In Canada,
from Olden Township, Frontenac County, Quebec; in the
McDonald mine, Hybla, Ontario; and at Hoidas Lake, near
Nisikkatch Lake, Saskatchewan. From near Telixtlahuaca,
Oaxaca, Mexico. In the Mary Kathleen mine, Queensland,
and at Broken Hill, New South Wales, Australia. From
Ribuae, Mozambique.
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