Bartonite
About Bartonite
See also chlorbartonite, rasvumite, gmalimite, 'Unnamed (K sulfides solid solution)', and UM1997-44-S:FeK.
Unique Identifiers
Similar Names
IMA Classification of Bartonite
Classification of Bartonite
2 : SULFIDES and SULFOSALTS (sulfides, selenides, tellurides; arsenides, antimonides, bismuthides; sulfarsenites, sulfantimonites, sulfbismuthites, etc.)
F : Sulfides of arsenic, alkalies; sulfides with halide, oxide, hydroxide, H2O
C : With Cl, Br, I (halide-sulfides)
2 : SULFIDES
9 : AmBnXp, with (m+n):p = 1:1
3 : Sulphides, Selenides, Tellurides, Arsenides and Bismuthides (except the arsenides, antimonides and bismuthides of Cu, Ag and Au, which are included in Section 1)
0 : Sulphides etc. of the alkalis
Mineral Symbols
| Symbol | Source | Reference for Standard |
|---|---|---|
| Btn | 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 Bartonite
Distinct on {112}
Optical Data of Bartonite
| Wavelength | R1 (%) | R2 (%) |
|---|---|---|
| 400nm | 21.7% | 18.3% |
| 420nm | 16.7% | 14.4% |
| 440nm | 17.7% | 17.2% |
| 460nm | 18.4% | 18.6% |
| 480nm | 19.4% | 19.5% |
| 500nm | 19.7% | 20.6% |
| 520nm | 20.3% | 21.4% |
| 540nm | 20.9% | 21.8% |
| 560nm | 21.9% | 22.7% |
| 580nm | 22.7% | 23.2% |
| 600nm | 23.4% | 23.7% |
| 620nm | 23.9% | 24.3% |
| 640nm | 24.7% | 25.1% |
| 660nm | 25.0% | 25.5% |
| 680nm | 25.2% | 26.1% |
| 700nm | 26.4% | 26.5% |
Graph shows reflectance levels at different wavelengths (in nm). Peak reflectance is 26.5%.
R1 shown in black, R2 shown in red
Chemistry of Bartonite
Crystallography of Bartonite
Crystal Structure
Unit Cell | Unit Cell Packed
2x2x2 | 3x3x3 | 4x4x4
Big Balls | Small Balls | Just Balls | Spacefill
Polyhedra Off | Si Polyhedra | All Polyhedra
Remove metal-metal sticks
Black Background | White Background
Perspective On | Perspective Off
2D | Stereo | Red-Blue | Red-Cyan
CIF File Best | x | y | z | a | b | c
Stop | Start
Console Off | On | Grey | Yellow
| ID | Species | Reference | Link | Year | Locality | Pressure (GPa) | Temp (K) |
|---|---|---|---|---|---|---|---|
| 0000824 | Bartonite | Evans H T, Clark J R (1981) The crystal structure of bartonite, a potassium iron sulfide, and its relationship to pentlandite and djerfisherite American Mineralogist 66 376-384 | ![]() | 1981 | 0 | 293 |
X-Ray Powder Diffraction
| d-spacing | Intensity |
|---|---|
| 9.31 Å | (27) |
| 5.99 Å | (77) |
| 3.139 Å | (27) |
| 2.998 Å | (100) |
| 2.379 Å | (25) |
| 1.841 Å | (25) |
| 1.833 Å | (40) |
Geological Environment
| Paragenetic Mode | Earliest Age (Ga) |
|---|---|
| High-? alteration and/or metamorphism | |
| 33 : Minerals deposited by hydrothermal metal-rich fluids (see also [#12]) | |
| Stage 4b: Highly evolved igneous rocks | >3.0 |
| 35 : Ultra-alkali and agpaitic igneous rocks |
Type Occurrence of Bartonite
Synonyms of Bartonite
Other Language Names for Bartonite
Relationship of Bartonite to other Species
| Djerfisherite Group | Structurally related to bartonite and pentlandite. |
Common Associates
Related Minerals - Strunz-mindat Grouping
| 2.FC. | Demicheleite-(I) | BiSI |
| 2.FC.05 | Djerfisherite | K6(Fe,Cu,Ni)25S26Cl |
| 2.FC.05 | Owensite | (Ba,Pb)6(Cu,Fe,Ni)25S27 |
| 2.FC.05 | Thalfenisite | Tl6(Fe,Ni,Cu)25S26Cl |
| 2.FC.05 | Gmalimite | K6◻Fe2+24S27 |
| 2.FC.05 | 'Cu-djerfisherite' | K6(Cu,Fe)25S26Cl |
| 2.FC.05 | Zoharite | (Ba,K)6(Fe,Cu,Ni)25S27 |
| 2.FC.10 | Chlorbartonite | K6Fe24S26(Cl,S) |
| 2.FC.15d | Radtkeite | Hg2+3S2ICl |
| 2.FC.15a | Lavrentievite | Hg3S2Cl2 |
| 2.FC.15a | Corderoite | Hg2+3S2Cl2 |
| 2.FC.15a | 'Arzakite' | Hg2+3S2(Br,Cl)2 |
| 2.FC.15c | Grechishchevite | Hg2+3S2(Br,Cl,I)2 |
| 2.FC.15b | Kenhsuite | Hg2+3S2Cl2 |
| 2.FC.20b | Iltisite | HgAgSCl |
| 2.FC.20c | Perroudite | Hg5Ag4S5(I,Br)2Cl2 |
| 2.FC.20a | Capgaronnite | AgHgClS |
| 2.FC.20d | Hanauerite | AgHgSI |
| 2.FC.25 | Demicheleite-(Cl) | BiSCl |
| 2.FC.25 | Demicheleite-(Br) | BiSBr |
Radioactivity
| Element | % Content | Activity (Bq/kg) | Radiation Type |
|---|---|---|---|
| Uranium (U) | 0.0000% | 0 | α, β, γ |
| Thorium (Th) | 0.0000% | 0 | α, β, γ |
| Potassium (K) | 10.5802% | 3,280 | β, γ |
For comparison:
- Banana: ~15 Bq per fruit
- Granite: 1,000–3,000 Bq/kg
- EU exemption limit: 10,000 Bq/kg
Note: Risk is shown relative to daily recommended maximum exposure to non-background radiation of 1000 µSv/year. Note that natural background radiation averages around 2400 µSv/year so in reality these risks are probably extremely overstated! With infrequent handling and safe storage natural radioactive minerals do not usually pose much risk.
Note: The mass selector refers to the mass of radioactive mineral present, not the full specimen, also be aware that the matrix may also be radioactive, possibly more radioactive than this mineral!
Activity: –
| Distance | Dose rate | Risk |
|---|---|---|
| 1 cm | ||
| 10 cm | ||
| 1 m |
The external dose rate (D) from a radioactive mineral is estimated by summing the gamma radiation contributions from its Uranium, Thorium, and Potassium content, disregarding daughter-product which may have a significant effect in some cases (eg 'pitchblende'). This involves multiplying the activity (A, in Bq) of each element by its specific gamma ray constant (Γ), which accounts for its unique gamma emissions. The total unshielded dose at 1 cm is then scaled by the square of the distance (r, in cm) and multiplied by a shielding factor (μshield). This calculation provides a 'worst-case' or 'maximum risk' estimate because it assumes the sample is a point source and entirely neglects any self-shielding where radiation is absorbed within the mineral itself, meaning actual doses will typically be lower. The resulting dose rate (D) is expressed in microsieverts per hour (μSv/h).
D = ((AU × ΓU) + (ATh × ΓTh) + (AK × ΓK)) / r2 × μshield
Other Information
Internet Links for Bartonite
Please feel free to link to this page.
References for Bartonite
Localities for Bartonite
Showing 13 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.
China | |
| Chen et al. (2014) |
Czech Republic | |
| Skála et al. (2015) |
Greenland | |
| Friis (2016) |
Italy | |
| Stoppa et al. (1997) +2 other references |
Jordan | |
| Sokol +9 other references |
Russia | |
| Spiridonov et al. (2016) |
| Pekov (2005) |
| Selivanova et al. (2024) |
| Kostin (2021) |
| Sharygin et al. (2010, September) | |
South Africa | |
| Abersteiner et al. (2024) |
USA (TL) | |
| Fleischer (1979) +5 other references |
| Castor et al. (2004) |







symbol to view information about a locality.
The
Coyote Peak, Humboldt County, California, USA