Chlorartinite
A valid IMA mineral species
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About Chlorartinite
Formula:
Mg2(CO3)(OH)Cl · 2H2O
Specific Gravity:
1.758 (Calculated)
Crystal System:
Trigonal
Name:
Chloride analog of artinite which was named after the Italian mineralogist E. Artini (1866-1928).
This page provides mineralogical data about Chlorartinite.
Unique Identifiers
Mindat ID:
6868
Long-form identifier:
mindat:1:1:6868:6
IMA Classification of Chlorartinite
Classification of Chlorartinite
5.DA.10
5 : CARBONATES (NITRATES)
D : Carbonates with additional anions, with H2O
A : With medium-sized cations
5 : CARBONATES (NITRATES)
D : Carbonates with additional anions, with H2O
A : With medium-sized cations
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 |
|---|---|---|
| Cart | 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 Chlorartinite
Density:
1.758 g/cm3 (Calculated)
Optical Data of Chlorartinite
Type:
Uniaxial
RI values:
nα = 1.51 nβ = 1.51
Max. Birefringence:
δ = 0.000
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:
Moderate
Comments:
Mean n = 1.503, delta n =< 0.006
Chemistry of Chlorartinite
Mindat Formula:
Mg2(CO3)(OH)Cl · 2H2O
Element Weights:
Crystallography of Chlorartinite
Crystal System:
Trigonal
Class (H-M):
3m - Ditrigonal Pyramidal
Space Group:
R3c
Cell Parameters:
a = 23.1442 Å, c = 7.22333 Å
Ratio:
a:c = 1 : 0.312
Unit Cell V:
3350.84 ų
Z:
18
Crystal Structure
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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) |
|---|---|---|---|---|---|---|---|
| 0019538 | Chlorartinite | Sugimoto K, Dinnebier R E, Schlecht T (2007) Crystal structure of dehydrated chlorartinite by X-ray powder diffraction Powder Diffraction 22 64-67 | 2007 | synthetic | 0 | 293 | |
| 0019537 | Chlorartinite | Sugimoto K, Dinnebier R E, Schlecht T (2006) Chlorartinite, a volcanic exhalation product also found in industrial magnesia screed Journal of Applied Crystallography 39 739-744 | 2006 | synthetic | 0 | 293 |
CIF Raw Data - click here to close
X-Ray Powder Diffraction
Powder Diffraction Data:
| d-spacing | Intensity |
|---|---|
| 11.66 Å | (100) |
| 3.264 Å | (21) |
| 3.218 Å | (21) |
| 3.000 Å | (41) |
| 2.657 Å | (22) |
Comments:
Tolbachik volcano, Russia. Data from type description.
Geological Environment
Paragenetic Mode(s):
| Paragenetic Mode | Earliest Age (Ga) |
|---|---|
| Stage 7: Great Oxidation Event | <2.4 |
| 45b : [Other oxidized fumarolic minerals] |
Geological Setting:
Serpentinized ultrabasics.
Type Occurrence of Chlorartinite
General Appearance of Type Material:
White, rounded, fine-grained aggregates.
Place of Conservation of Type Material:
Mineralogical Museum of Saint Petersburg Mining Institute, Russia.
Geological Setting of Type Material:
Fumarole.
Synonyms of Chlorartinite
Other Language Names for Chlorartinite
Related Minerals - Strunz-mindat Grouping
| 5.DA. | Alexkhomyakovite | K6(Ca2Na)(CO3)5Cl · 6H2O |
| 5.DA. | Amoraite | Ca12Al6(OH)36(CO3)2(SO3) · 15H2O |
| 5.DA.05 | Dypingite | Mg5(CO3)4(OH)2 · 5H2O |
| 5.DA.05 | 'UM1986-10-CO:ClHMgMnZn (also called Mineral F, Dunn, 1995)' | Mg5(Zn,Mn)3(CO3)2(OH,Cl)12 · H2O |
| 5.DA.05 | 'UM1987-01-CO:HMgS' | Mg4(CO3)2(OH)4 · 6H2O ? |
| 5.DA.05 | Giorgiosite | Mg5(CO3)4(OH)2 · 5-6H2O |
| 5.DA.05 | Hydromagnesite | Mg5(CO3)4(OH)2 · 4H2O |
| 5.DA.05 | Widgiemoolthalite | Ni5(CO3)4(OH)2 · 5H2O |
| 5.DA.10 | Artinite | Mg2(CO3)(OH)2 · 3H2O |
| 5.DA.10 | Indigirite | Mg2Al2(CO3)4(OH)2 · 15H2O |
| 5.DA.15 | Zaratite | Ni3(CO3)(OH)4 · 4H2O ? |
| 5.DA.15 | Otwayite | Ni2(CO3)(OH)2 · H2O |
| 5.DA.20 | Kambaldaite | NaNi4(CO3)3(OH)3 · 3H2O |
| 5.DA.25 | Callaghanite | Cu2Mg2(CO3)(OH)6 · 2H2O |
| 5.DA.30 | Claraite | (Cu,Zn)15(CO3)4(AsO4)2(SO4)(OH)14 · 7H2O |
| 5.DA.35 | Hydroscarbroite | Al14(CO3)3(OH)36 · nH2O |
| 5.DA.35 | Scarbroite | Al5(CO3)(OH)13 · 5H2O |
| 5.DA.40 | Karchevskyite | Mg18Al9(OH)54Sr2(CO3)9(H2O)6(H3O)5 |
| 5.DA.40 | 'UM1987-05-OH:AlCMg' | Mg4Al2(OH)12(CO3,SO4) · 3H2O |
| 5.DA.40 | Quintinite | Mg4Al2(OH)12(CO3) · 3H2O |
| 5.DA.40 | Charmarite | Mn2+4Al2(OH)12[CO3] · 3H2O |
| 5.DA.40 | Caresite | Fe2+4Al2(OH)12[CO3] · 3H2O |
| 5.DA.45 | 'Hydrotalcite-2H' | Mg6Al2(CO3)(OH)16 · 4H2O |
| 5.DA.45 | 'Stichtite-2H' | Mg6(Cr,Al)2(CO3)(OH)16 · 4H2O |
| 5.DA.45 | Brugnatellite | Mg6Fe3+(CO3)(OH)13 · 4H2O |
| 5.DA.45 | Zaccagnaite | Zn4Al2(OH)12[CO3] · 3H2O |
| 5.DA.45 | 'Pyroaurite-2H' | Mg6Fe3+2(OH)16(CO3) · 4H2O |
| 5.DA.45 | Liudongshengite | Zn4Cr2(OH)12(CO3) · 3H2O |
| 5.DA.45 | Chlormagaluminite | Mg4Al2(OH)12Cl2 · 3H2O |
| 5.DA.50 | Pyroaurite | Mg6Fe3+2(OH)16[CO3] · 4H2O |
| 5.DA.50 | Takovite | Ni6Al2(OH)16[CO3] · 4H2O |
| 5.DA.50 | Reevesite | Ni6Fe3+2(OH)16(CO3) · 4H2O |
| 5.DA.50 | Kaznakhtite | Ni6Co3+2(CO3)(OH)16 · 4H2O |
| 5.DA.50 | Comblainite | Ni4Co2(OH)12[CO3] · 3H2O |
| 5.DA.50 | Marioantofilliite | [Cu4Al2(OH)12](CO3) · 3H2O |
| 5.DA.50 | Hydrotalcite | Mg6Al2(CO3)(OH)16 · 4H2O |
| 5.DA.50 | Stichtite | Mg6Cr3+2(OH)16[CO3] · 4H2O |
| 5.DA.50 | Desautelsite | Mg6Mn3+2(OH)16[CO3] · 4H2O |
| 5.DA.55 | Coalingite | Mg10Fe3+2(OH)24[CO3] · 2H2O |
| 5.DA.55 | Akopovaite | Al4Li2(OH)12(CO3)(H2O)3 |
| 5.DA.60 | Šlikite | Zn2Mg(CO3)2(OH)2 · 4H2O |
| 5.DA.65 | Marklite | Cu5(CO3)2(OH)6 · 6H2O |
Other Information
IR Spectrum:
The infrared spectrum has absorption bands at 3720, 3680, and 1100 cm–1 (OH), 1530, 1445, and 840 cm–1 (CO3), and 705, 510, and 430 cm–1 [Mg(OH,Cl)].
Thermal Behaviour:
DTA gives endothermic peaks at 177°C (weak), 260°C (strong), 465°C (strong) and 490°C (weak).
The loss between 20–390°C was 20 wt% (H2O) and the loss from 390–1000°C was 28 wt% (Cl, CO2).
The loss between 20–390°C was 20 wt% (H2O) and the loss from 390–1000°C was 28 wt% (Cl, CO2).
Notes:
Stable in air. Slowly soluble in water. Readily soluble in weak acids.
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 Chlorartinite
mindat.org URL:
https://www.mindat.org/min-6868.html
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References for Chlorartinite
Reference List:
Sugimoto, Kunihisa, Dinnebier, Robert E., Schlecht, Thomas (2006) Chlorartinite, a volcanic exhalation product also found in industrial magnesia screed. Journal of Applied Crystallography, 39 (5). 739-744 doi:10.1107/s0021889806032109
Localities for Chlorartinite
Showing 5 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.
Costa Rica | |
| Garvie (2021) |
Poland | |
| Cu +2 other references |
Russia (TL) | |
| Vergasova et al. (1998) +1 other reference |
Spain | |
| Rewitzer et al. (2020) |
USA | |
| George W. Robinson and S.M. Carlson (2009) |
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The
Tolbachik Volcanic field, Milkovsky District, Kamchatka Krai, Russia