Triazolite
A valid IMA mineral species
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About Triazolite
Formula:
NaCu2(N3C2H2)2(NH3)2Cl3 · 4H2O
Colour:
Deep blue
Lustre:
Vitreous
Hardness:
2
Specific Gravity:
2.028 (Calculated)
Crystal System:
Orthorhombic
Name:
Named for the presence of 1,2,4-triazolate anions.
Chemically and structurally related to chanabayaite, for which it is a precursor phase. The second natural (mineral) triazolate to be discovered.
It is a metalorganic ammine complex in which 1,2,4-triazolate anion and ammonia molecule are ligands coordinating Cu2+.
It is a metalorganic ammine complex in which 1,2,4-triazolate anion and ammonia molecule are ligands coordinating Cu2+.
Unique Identifiers
Mindat ID:
51961
Long-form identifier:
mindat:1:1:51961:0
GUID
(UUID V4):
(UUID V4):
c076b7d0-7e35-4811-ac62-dcbe5602b279
IMA Classification of Triazolite
Approved
Approval year:
2017
First published:
2018
Type description reference:
Chukanov, Nikita V., Zubkova, Natalia V., Möhn, Gerhard, Pekov, Igor V., Belakovskiy, Dmitriy I., Van, Konstantin V., Britvin, Sergey N., Pushcharovsky, Dmitry Y. (2018) Triazolite, NaCu2(N3C2H2)2(NH3)2Cl3·4H2O, a new mineral species containing 1,2,4-triazolate anion, from a guano deposit at Pabellón de Pica, Iquique Province, Chile. Mineralogical Magazine, 82 (4) 1007-1014 doi:10.1180/minmag.2017.081.088
Classification of Triazolite
10.CA.50
10 : ORGANIC COMPOUNDS
C : Miscellaneous Organic Minerals
A : Miscellaneous Organic Minerals
10 : ORGANIC COMPOUNDS
C : Miscellaneous Organic Minerals
A : Miscellaneous Organic Minerals
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 |
---|---|---|
Tzl | 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 Triazolite
Vitreous
Transparency:
Translucent
Colour:
Deep blue
Streak:
Blue
Hardness:
2 on Mohs scale
Tenacity:
Brittle
Cleavage:
Perfect
Perfect on (001) and imperfect on (100) and (010).
Perfect on (001) and imperfect on (100) and (010).
Parting:
None observed.
Fracture:
Irregular/Uneven
Comment:
The fracture across the perfect cleavage plane is uneven.
Density:
2.028 g/cm3 (Calculated)
Optical Data of Triazolite
Type:
Biaxial (-)
RI values:
nα = 1.582(4) nβ = 1.625(3) nγ = 1.625(3)
2V:
Measured: 5° (3), Calculated: ~0°
Max Birefringence:
δ = 0.043
Image shows birefringence interference colour range (at 30µm thickness)
and does not take into account mineral colouration.
and does not take into account mineral colouration.
Surface Relief:
Moderate
Dispersion:
None observed.
Optical Extinction:
X = b.
Pleochroism:
Visible
Comments:
Distinct, Y = violet, X = Z = greenish-blue.
Comments:
Absorption: Y > X ≈ Z.
Chemistry of Triazolite
Mindat Formula:
NaCu2(N3C2H2)2(NH3)2Cl3 · 4H2O
Crystallography of Triazolite
Crystal System:
Orthorhombic
Class (H-M):
2 2 2 - Disphenoidal
Space Group:
P21 21 21
Cell Parameters:
a = 19.3575(5) Å, b = 7.15718(19) Å, c = 12.5020(4) Å
Ratio:
a:b:c = 2.705 : 1 : 1.747
Unit Cell V:
1732.09 ų
Z:
4
Morphology:
Prismatic crystals (up to 0.1 mm × 0.15 mm × 0.75 mm); Radial aggregates. Forms include pinacoids {001}, {010} and {100} and prisms {hk0} or {0kl}.
X-Ray Powder Diffraction
Powder Diffraction Data:
d-spacing | Intensity |
---|---|
10.22 Å | (97) |
6.135 Å | (40) |
5.696 Å | (17) |
5.182 Å | (59) |
5.119 Å | (100) |
4.854 Å | (19) |
3.294 Å | (18) |
2.202 Å | (18) |
Comments:
From Type Description.
Geological Environment
Paragenetic Mode(s):
Paragenetic Mode | Earliest Age (Ga) |
---|---|
Stage 10a: Neoproterozoic oxygenation/terrestrial biosphere | <0.6 |
52 : Guano- and urine-derived minerals | <0.4 |
Type Occurrence of Triazolite
General Appearance of Type Material:
Deep blue prismatic crystals up to 0.1 mm × 0.15 mm × 0.75 mm and their radial aggregates up to 1.5 mm across.
Place of Conservation of Type Material:
Type material is deposited in the collections of the Fersman Mineralogical Museum, Russian Academy of Sciences, Moscow, Russia, registration number 5037/1.
Empirical Formula of Type Material:
Na1.14(Cu1.86Fe0.14)(Cl2.99S0.23)N9.23C3.43H23.34O4.29
Chemical Analysis of Type Material:
Na | 4.91 % |
---|---|
Fe | 1.51 % |
Cu | 22.06 % |
Cl | 19.80 % |
S | 1.4 % |
C | 7.7 % |
H | 4.4 % |
N | 24.2 % |
O (calc.) | 12.83 % |
Total: | 98.81 % |
Geological Setting of Type Material:
In the contact zone between altered guano and the host rock, a gabbro consisting of amphibole, plagioclase minor clinochlore and accessory chalcopyrite.
Associated Minerals at Type Locality:
Reference:
Chukanov, N.V., Zubkova, N.V., Möhn, G., Pekov, I.V., Belakovskiy, D.I., Van, K.V., Britvin, S.N., Pushcharovsky, D.Y. (2018) Triazolite, NaCu2(N3C2H2)2(NH3)2Cl3·4H2O, a new mineral species containing 1,2,4-triazolate anion, from a guano deposit at Pabellón de Pica, Iquique Province, Chile. Mineralogical Magazine: 82: 1007-1014.
Synonyms of Triazolite
Common Associates
Associated Minerals Based on Photo Data:
4 photos of Triazolite associated with Chanabayaite | CuCl(N3C2H2)(NH3) · 0.25H2O |
3 photos of Triazolite associated with Joanneumite | Cu(C3N3O3H2)2(NH3)2 |
3 photos of Triazolite associated with Salammoniac | NH4Cl |
2 photos of Triazolite associated with Natroxalate | Na2(C2O4) |
1 photo of Triazolite associated with Ammineite | [CuCl2(NH3)2] |
1 photo of Triazolite associated with Halite | NaCl |
Related Minerals - Strunz-mindat Grouping
10.CA. | Tholins | (C,H,N) |
10.CA. | Natrosulfatourea | Na2(SO4)[CO(NH2)2] |
10.CA. | Allantoin | C4H6N4O3 |
10.CA. | Bojarite | Cu3(N3C2H2)3(OH)Cl2 · 6H2O |
10.CA.05 | Refikite | C20H32O2 |
10.CA.10 | Flagstaffite | C10H22O3 |
10.CA.15 | Hoelite | C14H8O2 |
10.CA.20 | Abelsonite | Ni(C31H32N4) |
10.CA.25 | Kladnoite | C6H4(CO)2NH |
10.CA.30 | Guanine | C5H5N5O |
10.CA.30 | Tinnunculite (of Chesnokov & Shcherbakova) | C10H12N8O8 |
10.CA.35 | Urea | CO(NH2)2 |
10.CA.40 | Uricite | C5H4N4O3 |
10.CA.45 | Chanabayaite | CuCl(N3C2H2)(NH3) · 0.25H2O |
10.CA.55 | Ernstburkeite | Mg(CH3SO3)2 · 12H2O |
10.CA.60 | Joanneumite | Cu(C3N3O3H2)2(NH3)2 |
10.CA.65 | Tinnunculite | C5H4N4O3 · 2H2O |
10.CA.70 | Dopplerite |
Fluorescence of Triazolite
Not fluorescent.
Other Information
IR Spectrum:
IR spectrum shows the presence of 1,2,4-triazolate anion and ammonia and water molecules.
Notes:
Triazolite dissolves in dilute HCl and HNO3 without gas evolution. It is insoluble in water, but crystals of triazolite become dull after exposure to warm water. Heating in a closed tube gives a white sublimate of NH4Cl. Melting is accompanied by the release of water and an additional portion of sublimate. Stronger heating results in reduction to metallic Cu.
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 Triazolite
mindat.org URL:
https://www.mindat.org/min-51961.html
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References for Triazolite
Reference List:
Hålenius, U., Hatert, F., Pasero, M., Mills, S. J. (2017) New minerals and nomenclature modifications approved in 2017, CNMNC Newsletter No 38. Mineralogical Magazine, 81 (4) 1033-1038 doi:10.1180/minmag.2017.081.062
Chukanov, Nikita V., Zubkova, Natalia V., Möhn, Gerhard, Pekov, Igor V., Belakovskiy, Dmitriy I., Van, Konstantin V., Britvin, Sergey N., Pushcharovsky, Dmitry Y. (2018) Triazolite, NaCu2(N3C2H2)2(NH3)2Cl3·4H2O, a new mineral species containing 1,2,4-triazolate anion, from a guano deposit at Pabellón de Pica, Iquique Province, Chile. Mineralogical Magazine, 82 (4) 1007-1014 doi:10.1180/minmag.2017.081.088
Localities for Triazolite
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).
Struck out - Mineral was erroneously reported from this locality.
Faded * - Never found at this locality but inferred to have existed at some point in the past (e.g. from pseudomorphs).
All localities listed without proper references should be considered as questionable.
All localities listed without proper references should be considered as questionable.
Chile (TL) | |
| Hålenius et al. (2017) +1 other reference |
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Pabellón de Pica, Chanabaya, Iquique Province, Tarapacá, Chile