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| Sadanagaite
was named to honor Professor Ryoichi Sadanaga of the
Mineralogical Institute, University of Tokyo, Tokyo,
Japan.
| Discovered
in 1980; IMA
status:
Valid (IMA Approved 1984) |
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Chemistry
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Chemical
Formula: |
(K,Na)Ca2(Fe2+,Mg,Al,Ti)5[(Si,Al)8O22](OH)2
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Potassium
Sodium Calcium Magnesium Aluminum Iron Silicate Hydroxide
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Molecular
Weight: |
931.99 gm
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Composition: |
Potassium |
3.15 % |
K |
3.79 % |
K2O |
|
Sodium |
0.62 % |
Na |
0.83 % |
Na2O |
|
Calcium |
8.60 % |
Ca |
12.03 % |
CaO |
|
Magnesium |
3.91 % |
Mg |
6.49 % |
MgO |
|
Titanium |
1.28 % |
Ti |
2.14 % |
TiO2 |
|
Aluminum |
7.96 % |
Al |
15.04 % |
Al2O3 |
|
Iron |
14.98 % |
Fe |
19.27 % |
FeO |
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Silicon |
18.08 % |
Si |
38.68 % |
SiO2 |
|
Hydrogen |
0.22 % |
H |
1.93 % |
H2O |
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Oxygen |
41.20 % |
O |
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|
|
100.00 % |
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100.21 % |
= 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/F.10-175
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Nickel-Strunz 10th
Ed. ID:
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9.DE.15
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9 : SILICATES (Germanates)
D : Inosilicates E : Inosilicates with 2-periodic double chains, Si4O11; Clinoamphiboles
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Related
to: |
Sadanagaite Root Name Group. Calcium Amphibole Subgroup.
w(OH, F, Cl)-dominant Amphibole Group. Amphibole Supergroup.
Magnesio-Sadanagaite - Sadanagaite
Series.
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Members
of Group: |
Sadanagaite Root Name Group:
Ferri-fluoro-sadanagaite, Ferri-sadanagaite, Ferro-ferri-fluoro-sadanagaite,
Ferro-ferri-sadanagaite, Ferro-fluoro-sadanagaite, Ferro-sadanagaite,
Fluoro-sadanagaite, Potassic-chloro-sadanagaite, Potassic-ferri-sadanagaite,
Potassic-ferro-chloro-sadanagaite, Potassic-ferro-ferri-sadanagaite,
Potassic-ferro-sadanagaite, Potassic-sadanagaite, Sadanagaite
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Varieties: |
None
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Synonyms: |
IMA1980-027,
Magnesiosadanagaite
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Crystal
Data
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Crystallography:
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Monoclinic
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Crystal
Habit:
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Prismatic
crystals, to 1 mm; as polycrystalline aggregates.
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Twinning:
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None
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Physical
Properties
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|
|
Cleavage: |
Perfect
on {110}
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Fracture: |
n/a
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Tenacity:
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Brittle
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Moh's
Hardness: |
~6.0
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Density:
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3.30 (g/cm3)
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Luminescence:
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None
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Radioactivity:
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Barely
Detectable;
GRapi = 44.72 (Gamma Ray American Petroleum Institute Units)
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Optical
Properties
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Color: |
Dark
brown to black; in thin section, paler with greater
silicon content
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Transparency: |
Semi-transparent to
opaque |
Luster: |
Vitreous |
Refractive
Index: |
1.673
- 1.697 Biaxial ( + ) or ( - )
|
Birefringence: |
0.024
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Dispersion: |
Perceptible; r > v |
Pleochroism: |
Strong; X
= pale brown, grayish, or greenish yellow; Y
= yellowish orange to light olive-brown; Z
= greenish brown, light olive-brown to dark yellowish
orange |
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Occurances
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Geological
Setting: |
By
contact metamorphism, producing banded skarns, under
amphibolite to pyroxene hornfels facies conditions;
from eclogites. |
Common
Associations: |
Vesuvianite,
Hercynite, Sphene, Ilmenite, Apatite (Yuge Island, Japan); Biotite, Orthoclase, subsilicic ferroan Pargasite (Nogo-Hakusan
area, Japan) |
Common
Impurities: |
Mn
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Type
Locality: |
Kasuga mine, Kasuga-mura, Ibigawa-cho, Gifu Prefecture, Chubu Region, Honshu Island, Japan
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Year
Discovered: |
1980
(IMA Approved 1984) |
View
mineral photos: |
Sadanagaite
Mineral Photos and Locations |
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Unusual
Gem Categories
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Black
Gems, Radioactive
Gems
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More
Information
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Mindat.org
Webmineral.com
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Sadanagaite
is a rare silicate mineral that is a silica-poor
member of the Calcium Amphibole Subgroup of minerals.
Technically speaking, Sadanagaite is a subsilicic, alumina-rich,
calcic amphibole. Sadanagaite
is also barely radioactive due to its potassium (K)
content. Sadanagaite
is actually considered a group name with over a dozen
members each varying slightly in their chemical
composition. The main differences between the members
are in the presence, or lack of, and the amounts of,
chlorine (Cl), flourine (F), iron (Fe) and potassium
(K). The result of these variations are names like Ferri-fluoro-sadanagaite
and Potassic-ferro-chloro-sadanagaite. Faceted
gems are very rare and are opaque, dark
brown to black with vitreous luster and Moh's hardness
of about 6.0. The only current source of gem sized crystals
is at Nusfjord, Flakstadøya Island, Flakstad, Lofoten, Nordland, Norway.
Sadanagaite
was discovered in 1980 at the Kasuga mine, Kasuga-mura, Ibigawa-cho, Gifu Prefecture, Chubu Region, Honshu Island, Japan
and approved by the IMA as
a new mineral species in 1984. Since then, the name
Sadanagaite has been given Group status and the Sadanagaite
Group has been redefined twice, in
the 1997 and 2012 IMA amphibole reports. Sadanagaite
was named to honor Professor Ryoichi Sadanaga of the
Mineralogical Institute, University of Tokyo, Tokyo,
Japan.
Sadanagaite
distribution: on
Yuge Island, Ehime Prefecture, and in the Nogo-Hakusan
area, Fukui Prefecture, Japan. At Nusfjord, Flakstadøya Island, Flakstad, Lofoten, Nordland, Norway.
At the Botallack mine, St. Just, Cornwall, England.
In the Oetztal, Austria.
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