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词条 Chanabayaite
释义

  1. Crystal structure

  2. Association

  3. Formation

  4. References

{{infobox mineral
| name = Chanabayaite
| category = Organic mineral
| image = File:Chanabayaite.jpg
| imagesize =
| alt =
| caption =
| formula = Cu2(N3C2H2Cl(NH3,Cl,H2O,[])4
| strunz =
| dana =
| system = Orthorhombic
| class = Dipyramidal (mmm)
H-M symbol: (2/m 2/m 2/m)
| symmetry = Imma
| unit cell = a = 19.48, b = 7.21,
c = 11.999 [Å] (approximated); Z = 4
| color = Blue
| colour =
| habit = Prisms (imperfect); radial aggregates
| twinning =
| cleavage = (001), perfect; (100) and (010), imperfect
| fracture =
| tenacity = Brittle
| mohs = 2
| luster =
| streak =
| diaphaneity =
| gravity =
| density = 1.48 (measured)
| polish =
| opticalprop =
| refractive =
| birefringence =
| pleochroism = Deep blue to pale blue with gray hue (strong)
| 2V =
| dispersion =
| extinction =
| length fast/slow =
| fluorescence =
| absorption =
| melt =
| fusibility =
| diagnostic =
| solubility =
| impurities =
| alteration =
| other =
| references = [1][2][3]
}}Chanabayaite is the first recognized triazolate mineral, having the following formula: Cu2(N3C2H2Cl(NH3,Cl,H2O,[])4. Minor iron admixture is also present.[2] It is also one of a few currently known minerals containing ammine groups, including also ammineite, joanneumite and shilovite.[4][5][6] All the minerals are rare and were found in a single guano deposit in Chile, called Pabellón de Pica.[7] A similar natural phase, formula NaCu2Cl3[N3C2H2]2[NH3]2·4H2O, likely a precursor of chanabayaite, is described by Zubkova et al. 2016.[8]

Crystal structure

The main features of the crystal structure of chanabayaite are:[2]

  • copper forms octahedra, part of which share corners
  • 1,2,4-triazolate anions link the octahedra

Association

Chanabayaite coexists with halite, joanneumite, nitratine, salammoniac and paragenetically-unrelated chalcopyrite. Chalcopyrite is present in an amphibole- and plagioclase-bearing gabbro, that conctacts the guano deposit.[2]

Formation

Three suggested processes account for the formation of chanabayaite:[2]

  • leaching of sodium from the precursor phase
  • leaching of chlorine from the precursor phase
  • partial dehydratation of the precursor phase

References

1. ^[https://www.mineralienatlas.de/lexikon/index.php/MineralData?mineral=Chanabayaite Mineralienatlas]
2. ^Chukanov, N.V., Zubkova, N.V., Möhn, G., Pekov, I.V., Pushcharovsky, D.Yu., and Zadov, A.E., 2015. Chanabayaite, Cu2(N3C2H2Cl(NH3,Cl,H2O,[])4, a new mineral containing triazolate anion. Geology of Ore Deposits 57(8), 712-720.
3. ^{{cite web|url=http://www.mindat.org/min-43945.html |title=Chanabayaite: Chanabayaite mineral information and data |website=Mindat.org |accessdate=2016-03-10}}
4. ^{{cite web|url=http://www.mindat.org/min-38895.html |title=Ammineite: Ammineite mineral information and data |website=Mindat.org |accessdate=2016-03-10}}
5. ^{{cite web|url=http://www.mindat.org/min-42755.html |title=Joanneumite: Joanneumite mineral information and data |website=Mindat.org |accessdate=2016-03-10}}
6. ^{{cite web|url=http://www.mindat.org/min-46139.html |title=Shilovite: Shilovite mineral information and data |website=Mindat.org |accessdate=2016-03-10}}
7. ^{{cite web|url=http://www.mindat.org/min-43945.html |title=Chanabayaite: Chanabayaite mineral information and data |website=Mindat.org |accessdate=2016-03-10}}
8. ^Zubkova, N.V., Chukanov, N.V., Pekov, I., and Pushcharovsky, D., 2016. The crystal structure of the natural 1,2,4-triazolate compound NaCu2Cl3[N3C2H2]2[NH3]2·4H2O. Zeitschrift für Kristallographie - Crystalline Materials 231(1), 47–53.

3 : Copper minerals|Organic minerals|Orthorhombic minerals

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