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Kinichilite

A valid IMA mineral species
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About KinichiliteHide

06066860017271924403440.jpg
Dr. Kinichi Sakurai
Formula:
Mg0.5Mn2+Fe3+(Te4+O3)3 · 4.5H2O
Colour:
Dark Brown
Lustre:
Sub-Adamantine
Hardness:
2
Specific Gravity:
4.11 (Calculated)
Crystal System:
Hexagonal
Member of:
Name:
Named in 1981 by Hidemichi Hori, Eiji Koyama, and Kozo Nagashima in honor of Dr. Kin-ichi Sakurai (December 11, 1912, Tokyo – October 6, 1993), amateur mineralogist of Tokyo. He described and/or provided type material for half a dozen species. The mineral sakuraiite is also named in his honor.

Unique IdentifiersHide

Mindat ID:
2212
Long-form identifier:
mindat:1:1:2212:1

Similar NamesHide

IMA Classification of KinichiliteHide

Approved
IMA Formula:
Mg0.5Mn2+Fe3+(Te4+O3)3·4.5H2O
Approval year:
1979
First published:
1981

Classification of KinichiliteHide

4.JM.05

4 : OXIDES (Hydroxides, V[5,6] vanadates, arsenites, antimonites, bismuthites, sulfites, selenites, tellurites, iodates)
J : Arsenites, antimonites, bismuthites, sulfites, selenites, tellurites; iodates
M : Tellurites without additional anions, with H2O
34.3.2.2

34 : SELENITES, TELLURITES AND SULFITES
3 : A2(XO3)3·xH2O
28.3.9

28 : Selenites, Selenates, Tellurites, and Tellurates
3 : Tellurites

Mineral SymbolsHide

As of 2021 there are now IMA–CNMNC approved mineral symbols (abbreviations) for each mineral species, useful for tables and diagrams.

SymbolSourceReference for Standard
KniIMA–CNMNCWarr, L.N. (2021). IMA–CNMNC approved mineral symbols. Mineralogical Magazine, 85(3), 291-320. doi:10.1180/mgm.2021.43

Physical Properties of KinichiliteHide

Sub-Adamantine
Transparency:
Translucent
Colour:
Dark Brown
Streak:
Brown
Hardness:
Tenacity:
Fragile
Cleavage:
None Observed
Density:
4.11 g/cm3 (Calculated)

Optical Data of KinichiliteHide

Type:
Uniaxial (+)
RI values:
nω = 1.8 nε = 1.8
Surface Relief:
Very High (positive)
Relative to Canada balsam mounting medium (n ≈ 1.537).

This shows the grain boundary and Becke line effect under plane-polarised light, based on the contrast between this mineral's average refractive index and the mounting medium. It does not take into account mineral colouration.
In focus
Interference Figure:
This shows the idealized uniaxial interference figure - the conoscopic (convergent-light, Bertrand-lens-in) view, for a grain cut with the optic axis centred and vertical. The coloured rings are isochromatics, computed with the same physics as the Michel-Lévy bar above; the dark cross is the isogyre.

For a genuinely uniaxial mineral viewed this way, that cross stays perfectly stationary if you rotate the stage - unlike a biaxial mineral, where it splits apart on rotation. That invariance is itself the standard diagnostic test for telling uniaxial and biaxial minerals apart at the microscope.
Pleochroism:
Weak
Comments:
Pale brown to yellowish brown
Comments:
Indices => 1.8

Chemistry of KinichiliteHide

Mindat Formula:
Mg0.5Mn2+Fe3+(Te4+O3)3 · 4.5H2O
Element Weights:
Element% weight
Te52.381 %
O29.556 %
Fe7.642 %
Mn7.518 %
Mg1.663 %
H1.241 %

Calculated from ideal end-member formula.
Te
O
Fe
Mn
Mg
H

Crystallography of KinichiliteHide

Crystal System:
Hexagonal
Class (H-M):
6/m - Dipyramidal
Space Group:
P63/m
Cell Parameters:
a = 9.451(7) Å, c = 7.687(3) Å
Ratio:
a:c = 1 : 0.813
Unit Cell V:
594.62 ų (Calculated from Unit Cell)
Z:
2
Morphology:
Imperfect hexagonal prisms to 2mm.

Crystal StructureHide

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IDSpeciesReferenceLinkYearLocalityPressure (GPa)Temp (K)
0006593KinichiliteMiletich F (1995) Crystal chemistry of the microporous tellurite minerals zemannite and kinichilite, Mg0.5[MeFe(TeO3)3].4.5H2O, (Me=Zn;Mn) European Journal of Mineralogy 7 509-5231995Kawazu Mine, Rendaiji, Shimoda City, Shizuoka Prefecture, Japan0293
CIF Raw Data - click here to close

X-Ray Powder DiffractionHide

Powder Diffraction Data:
d-spacingIntensity
4.079 Å(100)
8.15 Å(90)
2.790 Å(85)
2.861 Å(50)
3.824 Å(35)
2.966 Å(30)
1.735 Å(20)

Geological EnvironmentHide

Paragenetic Mode(s):
Paragenetic ModeEarliest Age (Ga)
Stage 7: Great Oxidation Event<2.4
47a : [Near-surface hydration of prior minerals]
47e : [Vanadates, chromates, manganates]

Type Occurrence of KinichiliteHide

General Appearance of Type Material:
Hexagonal prisms to 2 mm.
Place of Conservation of Type Material:
National Science Museum, Tokyo, Japan, M-23380.
National Museum of Natural History, Washington, D.C., USA, 164269.
Geological Setting of Type Material:
Oxidation zone of low temperature hydrothermal Au-Ag-Te quartz veins.
Associated Minerals at Type Locality:

Synonyms of KinichiliteHide

Other Language Names for KinichiliteHide

Relationship of Kinichilite to other SpeciesHide

Member of:
Other Members of Zemannite Group:
IlirneyiteMg0.5ZnMn3+(Te4+O3)3 · 4.5H2OHex. 6/m : P63/m
KeystoneiteMg0.5Ni2+Fe3+(Te4+O3)3 · 4.5H2OHex. 6 : P63
ZemanniteMg0.5ZnFe3+(Te4+O3)3 · 4.5H2OTrig. 3 : P3

Common AssociatesHide

Associations Based on Photo Data:
1 photo of Kinichilite associated with QuartzSiO2

Related Minerals - Strunz-mindat GroupingHide

4.JM.WortupaiteMgNi2+2(Te4+O3)3 · 3H2OHex. 6/m : P63/m
4.JM.RudolfhermanniteFe3+2(Te4+O3)3(H2O)Hex. 6/m : P63/m
4.JM.05ZemanniteMg0.5ZnFe3+(Te4+O3)3 · 4.5H2OTrig. 3 : P3
4.JM.05KeystoneiteMg0.5Ni2+Fe3+(Te4+O3)3 · 4.5H2OHex. 6 : P63
4.JM.05IlirneyiteMg0.5ZnMn3+(Te4+O3)3 · 4.5H2OHex. 6/m : P63/m
4.JM.10EmmonsiteFe3+2(TeO3)3 · 2H2OTric. 1 : P1
4.JM.10BlakeiteFe3+2[TeO3]3 (?)
4.JM.15GraemiteCu[TeO3] · H2OOrth. mmm(2/m2/m2/m) : Pmma
4.JM.20TelluromandarinoiteFe3+2Te3O9 · 6H2OMon. 2/m : P21/c
4.JM.20TeineiteCu2+(Te4+O3) · 2H2OOrth. 222 : P212121
4.JM.25MillsiteCu2+(Te4+O3) · 2H2OMon. 2/m : P21/c

Other InformationHide

Notes:
Readily soluble in HCl and HNO3.
Health Risks:
No information on health risks for this material has been entered into the database. You should always treat mineral specimens with care.

Internet Links for KinichiliteHide

References for KinichiliteHide