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| Kryzhanovskite
was named to honor Vladimir Il’ich Kryzhanovskii (1881–1947),
Russian mineralogist, Curator of the A.E. Fersman Mineralogical
Museum, Academy of Sciences, Moscow, Russia.
| Discovered
in 1950; IMA
status:
Valid (pre-IMA; Grandfathered) |
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Chemistry
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Chemical
Formula: |
Mn2+Fe23+(PO4)2(OH)2
•
(H2O) |
|
Hydrated
Manganese Iron Phosphate Hydroxide |
Molecular
Weight: |
408.60 gm
|
Composition: |
Manganese |
13.45 % |
Mn |
17.36 % |
MnO |
|
Iron |
27.34 % |
Fe |
39.08 % |
Fe2O3 |
|
Phosphorus |
15.16 % |
P |
34.74 % |
P2O5 |
|
Hydrogen |
0.99 % |
H |
8.82 % |
H2O |
|
Oxygen |
43.07 % |
O |
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|
|
100.00 % |
|
100.00 % |
= TOTAL OXIDE |
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Classification
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Mineral
Classification: |
Phosphates
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Strunz 8th
Ed. ID:
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7/C.08-40
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Nickel-Strunz 10th
Ed. ID:
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8.CC.05
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8 : PHOSPHATES, ARSENATES, VANADATES
C : Phosphates without additional anions, with H2O
C : With only medium-sized cations, RO4:H2O = 1:1.5
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Related
to: |
Phosphoferrite Group.
Garyansellite-Kryzhanovskite Series.
Can be derived from Phosphoferrite by oxidation.
|
Members
of Group: |
Phosphoferrite Group:
Correianevesite, Garyansellite, Kryzhanovskite, Landesite,
Phosphoferrite, Reddingite
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Varieties: |
None
|
Synonyms: |
ICSD 303,
Kruzhanovskite, Kryjanovskite, PDF 24-731
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Crystal
Data
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Crystallography:
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Orthorhombic - Dipyramidal
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Crystal
Habit:
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Crystals
are typically rough pseudo-octahedra, prismatic or as
plates flattened on {010}, to 5 cm; may be granular.
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Twinning:
|
None
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Physical
Properties
|
|
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Cleavage: |
Perfect
on {001}
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Fracture: |
Irregular/Uneven
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Tenacity:
|
Brittle
|
Moh's
Hardness: |
3.5
- 4.0
|
Density:
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3.31 (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: |
Deep
red-brown, dark blackish brown to light golden-brown,
bronze on cleavage surfaces
|
Transparency: |
Opaque
to translucent |
Luster: |
Vitreous to
dull |
Refractive
Index: |
1.79
- 1.82 Biaxial ( + )
|
Birefringence: |
0.030
|
Dispersion: |
Strong; r
< v or r > v |
Pleochroism: |
Strong; X
= wine-yellow; Y
= orange-brown; Z
= reddish brown |
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Occurances
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Geological
Setting: |
A
rare low-temperature oxidation product of phosphate
minerals in complex granite pegmatites and iron formations.
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Common
Associations: |
Sicklerite,
Triphylite (Kalba Range, Kazakhstan); Ferrisicklerite,
Triphylite (Clementine II pegmatite, Namibia); Garyansellite,
Ludlamite, Arrojadite, Vivianite, Metavivianite, Souzalite,
Quartz (Rapid Creek, Canada) |
Common
Impurities: |
None
|
Type
Locality: |
Ak-Kezen' pegmatite,
Belogorskii Town, Kalba Range, Eastern Kazakhstan Province (Shyghys
Qazaqstan Oblysy; Vostochno-Kazakhstanskaya Oblast'), Kazakhstan |
Year
Discovered: |
1950
|
View
mineral photos: |
Kryzhanovskite
Mineral Photos and Locations |
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More
Information
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|
Mindat.org
Webmineral.com
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|
Kryzhanovskite
is a rare phophate mineral that is a member of the Phosphoferrite Group
of minerals. Crystals are typically opaque to translucent,
deep
red-brown, dark blackish brown to light golden-brown,
with a vitreous to dull luster and Moh's hardness of
3.5 - 4. Kryzhanovskite was discovered at the Ak-Kezen' pegmatite,
Belogorskii Town, Kalba Range, Eastern Kazakhstan Province, Kazakhstan and named to honor Vladimir Il’ich Kryzhanovskii (1881–1947),
Russian mineralogist, Curator of the A.E. Fersman Mineralogical
Museum, Academy of Sciences, Moscow, Russia. The picture
above shows a dark blackish brown faceted gem from the
east side of Rapid Creek, one km north of Lake
Creek, Yukon Territory, Canada.
Kryzhanovskite
distribution: from
[the Ak-Kezen’ pegmatites,] near Belogorskii, Kalba
Range, Kazakhstan. Abundant at the Clementine II pegmatite,
Okatjimukuju farm, near Karibib, Namibia. Large crystals
on the east side of Rapid Creek, one km north of Lake
Creek, Yukon Territory, Canada. In the USA, in South
Dakota, from the Bull Moose, Dan Patch, and Ferguson
mines, near Keystone, and the Big Chief mine, one km
south of Glendale, Pennington County; from the Tip Top
mine, 8.5 km southwest of Custer, Custer County; in
the Palermo #1 mine, near North Groton, Grafton County,
New Hampshire. At Hagendorf, Bavaria, Germany. From
the Bendada pegmatite, near Guarda, and in the Mangualde
pegmatite, near Mesquitela, Portugal. From the Pinilla
de Fermoselle pegmatite, Zamora, Spain.
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