Khinite
A valid IMA mineral species
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About Khinite
Formula:
Pb2+Cu2+3[Te6+O6](OH)2
Colour:
Dark green to bottle green
Lustre:
Vitreous
Hardness:
3
Specific Gravity:
6.5 - 7.0
Crystal System:
Orthorhombic
Name:
Named in honor of BaSaw Khin (b. 1931, Burma), a mineralogist with Phelps Dodge Corporation, USA. He found the first specimens of parakhinite.
Two polytypes are known, khinite-4O (orthorhombic) and khinite-3T (trigonal). The two polytypes have different stackings of otherwise identical layers of composition [Cu3(TeO6)(OH)2]2-, with Pb2+ cations between the layers.
Unique Identifiers
Mindat ID:
2199
Long-form identifier:
mindat:1:1:2199:5
Similar Names
IMA Classification of Khinite
Approved
IMA Formula:
Cu2+3Pb2+Te6+O6(OH)2
Approval year:
1978
First published:
1978
Classification of Khinite
4.FD.30
4 : OXIDES (Hydroxides, V[5,6] vanadates, arsenites, antimonites, bismuthites, sulfites, selenites, tellurites, iodates)
F : Hydroxides (without V or U)
D : Hydroxides with OH, without H2O; chains of edge-sharing octahedra
4 : OXIDES (Hydroxides, V[5,6] vanadates, arsenites, antimonites, bismuthites, sulfites, selenites, tellurites, iodates)
F : Hydroxides (without V or U)
D : Hydroxides with OH, without H2O; chains of edge-sharing octahedra
Dana 7th ed.:
33.1.3.1
33.1.3.1
33 : SELENATES AND TELLURATES
1 : (AB)m(XO4)pZq
33 : SELENATES AND TELLURATES
1 : (AB)m(XO4)pZq
28.4.8
28 : Selenites, Selenates, Tellurites, and Tellurates
4 : Tellurates
28 : Selenites, Selenates, Tellurites, and Tellurates
4 : Tellurates
Mineral Symbols
As of 2021 there are now IMA–CNMNC approved mineral symbols (abbreviations) for each mineral species, useful for tables and diagrams.
| Symbol | Source | Reference for Standard |
|---|---|---|
| Khn | IMA–CNMNC | Warr, L.N. (2021). IMA–CNMNC approved mineral symbols. Mineralogical Magazine, 85(3), 291-320. doi:10.1180/mgm.2021.43 |
Physical Properties of Khinite
Vitreous
Transparency:
Translucent
Colour:
Dark green to bottle green
Streak:
Vivid green
Hardness:
3 on Mohs scale
Tenacity:
Brittle
Cleavage:
Imperfect/Fair
On {001}
On {001}
Density:
6.5 - 7.0 g/cm3 (Measured) 6.29 g/cm3 (Calculated)
Comment:
Thoulet's method
Optical Data of Khinite
Type:
Biaxial (+)
RI values:
nα = 2.11 nβ = 2.112 nγ = 2.165
2V:
Measured: 20° , Calculated: 24°
Max. Birefringence:
δ = 0.055
Based on recorded range of RI values above.
Based on recorded range of RI values above.
Interference Colours:
The colours simulate birefringence patterns seen in thin section under crossed polars. They do not take into account mineral colouration or opacity.
Michel-Levy Bar The default colours simulate the birefringence range for a 30 µm thin-section thickness. Adjust the slider to simulate a different thickness.
Grain Simulation You can rotate the grain simulation to show how this range might look as you rotated a sample under crossed polars. Each grain retains its interference colour (retardation) while its brightness falls to black at extinction and reaches a maximum between extinction positions.
The colours simulate birefringence patterns seen in thin section under crossed polars. They do not take into account mineral colouration or opacity.
Michel-Levy Bar The default colours simulate the birefringence range for a 30 µm thin-section thickness. Adjust the slider to simulate a different thickness.
Grain Simulation You can rotate the grain simulation to show how this range might look as you rotated a sample under crossed polars. Each grain retains its interference colour (retardation) while its brightness falls to black at extinction and reaches a maximum between extinction positions.
Surface Relief:
Very High (positive)
Relative to Canada balsam mounting medium (n ≈ 1.537).
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 biaxial acute bisectrix (Bxa) interference figure
- the conoscopic view for a grain cut perpendicular to the acute bisectrix, using
this mineral's 2V. The two small white dots mark the melatopes - the points
where the two optic axes emerge - and are shown only when they fall within the
field of view. The coloured bands are isochromatics, and the dark bands are
isogyres.
Rotate the stage: at 0°/90° the isogyres form a cross through the melatopes; at 45° they pull apart into curved hyperbolas. That splitting on rotation - absent in a uniaxial figure - is the standard diagnostic test for telling biaxial minerals from uniaxial ones. If 2V is large, the melatopes may fall outside the field of view, as they often do at the microscope too.
Rotate the stage: at 0°/90° the isogyres form a cross through the melatopes; at 45° they pull apart into curved hyperbolas. That splitting on rotation - absent in a uniaxial figure - is the standard diagnostic test for telling biaxial minerals from uniaxial ones. If 2V is large, the melatopes may fall outside the field of view, as they often do at the microscope too.
Dispersion:
strong
Pleochroism:
Visible
Comments:
Rich yellowish green (Y,Z), vivid emerald green (X)
Z = Y > X
Z = Y > X
Chemistry of Khinite
Mindat Formula:
Pb2+Cu2+3[Te6+O6](OH)2
Element Weights:
Crystallography of Khinite
Polytype:
Formula:
Crystal System:
Class (H-M)
Space Group:
Space Group Setting:
Cell Parameters:
Ratio:
Unit Cell Volume (calc):
Z:
Comment:
| Khinite-3T | Khinite-4O |
|---|---|
| Pb2+Cu2+3Te6+O6(OH)2 | Pb2+Cu2+3[Te6+O6](OH)2 |
| Trigonal | Orthorhombic |
| 3 - Pyramidal | mm2 - Pyramidal |
| P32 | Fdd2 |
| a = 5.765(2) Å, c = 18.001(9) Å | a = 5.7491(10) Å, b = 10.0176(14) Å, c = 24.022(3) Å |
| a:c = 1 : 3.122 | a:b:c = 0.574 : 1 : 2.398 |
| V 518 ų | V 1383.6 ų |
| 3 | 8 |
Crystal Structure
Load
Unit Cell | Unit Cell Packed
2x2x2 | 3x3x3 | 4x4x4
Unit Cell | Unit Cell Packed
2x2x2 | 3x3x3 | 4x4x4
Show
Big Balls | Small Balls | Just Balls | Spacefill
Polyhedra Off | Si Polyhedra | All Polyhedra
Remove metal-metal sticks
Big Balls | Small Balls | Just Balls | Spacefill
Polyhedra Off | Si Polyhedra | All Polyhedra
Remove metal-metal sticks
Display Options
Black Background | White Background
Perspective On | Perspective Off
2D | Stereo | Red-Blue | Red-Cyan
Black Background | White Background
Perspective On | Perspective Off
2D | Stereo | Red-Blue | Red-Cyan
View
CIF File Best | x | y | z | a | b | c
CIF File Best | x | y | z | a | b | c
Rotation
Stop | Start
Stop | Start
Labels
Console Off | On | Grey | Yellow
Console Off | On | Grey | Yellow
Data courtesy of the American Mineralogist Crystal Structure Database. Click on an AMCSD ID to view structure
| ID | Species | Reference | Link | Year | Locality | Pressure (GPa) | Temp (K) |
|---|---|---|---|---|---|---|---|
| 0014584 | Khinite | Cooper M A, Hawthorne F C, Back M E (2008) The crystal structure of khinite and polytypism in khinite and parakhinite Mineralogical Magazine 72 763-770 | 2008 | the Empire mine, Tombstone, Arizona, USA | 0 | 293 | |
| 0014583 | Khinite | Cooper M A, Hawthorne F C, Back M E (2008) The crystal structure of khinite and polytypism in khinite and parakhinite Mineralogical Magazine 72 763-770 | 2008 | the Empire mine, Tombstone, Arizona, USA | 0 | 293 | |
| 0005428 | Khinite | Burns P C, Cooper M A, Hawthorne F C (1995) Parakhinite, Cu3PbTeO6(OH)2: Crystal structure and revision of chemical formula formerly known as parakhinite The Canadian Mineralogist 33 33-40 | ![]() | 1995 | 0 | 293 |
CIF Raw Data - click here to close
Geological Environment
Paragenetic Mode(s):
| Paragenetic Mode | Earliest Age (Ga) |
|---|---|
| Stage 7: Great Oxidation Event | <2.4 |
| 47a : [Near-surface hydration of prior minerals] | |
| 47e : [Vanadates, chromates, manganates] |
Type Occurrence of Khinite
General Appearance of Type Material:
Deeply etched curved or barrel shaped bipyramids.
Place of Conservation of Type Material:
The Natural History Museum, London, England, numbers 1980,541 and 1980,543.
National Museum of Natural History, Washington, D.C., USA, numbers 164352.
National Museum of Natural History, Washington, D.C., USA, numbers 164352.
Geological Setting of Type Material:
Tellurium-bearing dumps.
Associated Minerals at Type Locality:
Synonyms of Khinite
Other Language Names for Khinite
Common Associates
Associations Based on Photo Data:
| 35 photos of Khinite associated with Quartz | SiO2 |
| 34 photos of Khinite associated with Timroseite | Pb2Cu5(TeO6)2(OH)2 |
| 33 photos of Khinite associated with Native Gold | Au |
| 28 photos of Khinite associated with Thorneite | Pb6(Te6+2O10)(CO3)Cl2(H2O) |
| 11 photos of Khinite associated with Chlorargyrite | AgCl |
| 8 photos of Khinite associated with Cerussite | PbCO3 |
| 6 photos of Khinite associated with Wulfenite | Pb(MoO4) |
| 5 photos of Khinite associated with Markcooperite | Pb2(UO2)(TeO6) |
| 5 photos of Khinite associated with Housleyite | Pb6CuTe6+4O18(OH)2 |
| 4 photos of Khinite associated with Eckhardite | (Ca,Pb)Cu2+Te6+O5(H2O) |
Related Minerals - Strunz-mindat Grouping
| 4.FD.05 | Spertiniite | Cu(OH)2 |
| 4.FD.10 | Diaspore | AlO(OH) |
| 4.FD.10 | Goethite | Fe3+O(OH) |
| 4.FD.10 | Montroseite | (V3+,Fe3+)O(OH) |
| 4.FD.10 | Tsumgallite | GaO(OH) |
| 4.FD.10 | Groutite | Mn3+O(OH) |
| 4.FD.10 | Bracewellite | CrO(OH) |
| 4.FD.10 | Guyanaite | CrO(OH) |
| 4.FD.15 | Manganite | Mn3+O(OH) |
| 4.FD.20 | Yttrotungstite-(Y) | YW2O7(OH) · H2O |
| 4.FD.20 | Yttrotungstite-(Ce) | CeW2O7(OH) · H2O |
| 4.FD.25 | Frankhawthorneite | Cu2Te6+O4(OH)2 |
| 4.FD.30 | 'Khinite-3T' | Pb2+Cu2+3Te6+O6(OH)2 |
| 4.FD.30 | Housleyite | Pb6CuTe6+4O18(OH)2 |
Fluorescence of Khinite
None
Other Information
Notes:
Quickly dissolves in even mildly alkaline water.
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 Khinite
mindat.org URL:
https://www.mindat.org/min-2199.html
Please feel free to link to this page.
Please feel free to link to this page.
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Mineral Dealers:
References for Khinite
Reference List:
Williams, S. A. (1978) Khinite, parakhinite, and dugganite, three new tellurates from Tombstone, Arizona. American Mineralogist, 63 (9-10) 1016-1019
Cooper, M. A., Hawthorne, F. C., Back, M. E. (2008) The crystal structure of khinite and polytypism in khinite and parakhinite. Mineralogical Magazine, 72 (3) 763-770 doi:10.1180/minmag.2008.072.3.763
Localities for Khinite
Showing 30 localities.
Locality List
- This locality has map coordinates listed.
- This locality has estimated coordinates.
ⓘ - Click for references and further information on this occurrence.
? - Indicates mineral may be doubtful at this locality.
- Good crystals or important locality for species.
- World class for species or very significant.
(TL) - Type Locality for a valid mineral species.
(FRL) - First Recorded Locality for everything else (eg varieties).
All localities listed without proper references should be considered as questionable.
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The
Bird Nest drift, Otto Mountain, Baker, Soda Mountains, Silver Lake Mining District, San Bernardino County, California, USA