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Yazganite

A valid IMA mineral species
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Formula:
NaFe3+2(Mg,Mn2+)(AsO4)3 · H2O
Colour:
Brown to brown-black
Lustre:
Adamantine, Metallic
Hardness:
5
Specific Gravity:
4.18
Crystal System:
Monoclinic
Name:
For Dr. Evren Yazgan (1943-), Turkish geologist, who collected the samples containing the mineral.
Alluaudite Group.

Structure is a variant of the Johillerite structure. The first hydrated mineral in this group.


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Unique IdentifiersHide

Mindat ID:
27522
Long-form identifier:
mindat:1:1:27522:0

IMA Classification of YazganiteHide

Approved
IMA Formula:
◻NaMgFe3+2(As5+O4)3·H2O
Approval year:
2003
First published:
2005

Classification of YazganiteHide

8.CF.10

8 : PHOSPHATES, ARSENATES, VANADATES
C : Phosphates without additional anions, with H2O
F : With large and medium-sized cations, RO4:H2O > 1:1
Dana 7th ed.:
38.2.7.5

Mineral SymbolsHide

As of 2021 there are now IMA–CNMNC approved mineral symbols (abbreviations) for each mineral species, useful for tables and diagrams.

SymbolSourceReference for Standard
YazIMA–CNMNCWarr, L.N. (2021). IMA–CNMNC approved mineral symbols. Mineralogical Magazine, 85(3), 291-320. doi:10.1180/mgm.2021.43

Physical Properties of YazganiteHide

Adamantine, Metallic
Transparency:
Translucent
Colour:
Brown to brown-black
Streak:
Bright brown to yellow-gray
Hardness:
Tenacity:
Brittle
Cleavage:
None Observed
Fracture:
Conchoidal
Density:
4.18 g/cm3 (Measured)    4.19 g/cm3 (Calculated)

Optical Data of YazganiteHide

Type:
Biaxial (-)
RI values:
nα = 1.870 nβ = 1.897 nγ = 1.900
2V:
Measured: 35° , Calculated: 36.5°
Max. Birefringence:
δ = 0.030
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.

Surface Relief:
Moderate
Optical Extinction:
X ∧ a = 5°, Y = b, Z ∧ c = 17°.
Pleochroism:
Visible
Comments:
Moderate. α = orange brown, yellow; γ = β = grayish yellow, colorless.

Chemistry of YazganiteHide

Mindat Formula:
NaFe3+2(Mg,Mn2+)(AsO4)3 · H2O
Element Weights:
Element% weight
As37.855 %
O35.030 %
Fe18.811 %
Mg4.093 %
Na3.872 %
H0.340 %

Calculated from ideal end-member formula.

Crystallography of YazganiteHide

Crystal System:
Monoclinic
Class (H-M):
2/m - Prismatic
Space Group:
B2/b
Cell Parameters:
a = 12.181 Å, b = 12.807 Å, c = 6.6391 Å
β = 112.441°
Ratio:
a:b:c = 0.951 : 1 : 0.518
Unit Cell V:
957.28 ų (Calculated from Unit Cell)
Z:
4
Morphology:
Isolated prismatic crystals or aggregates. Type material: Prismatic crystals are elongated on [001], flattened on {010} with forms {010}, {100}, {110}, {131}, {111}, and {311}.
Twinning:
Not observed.

Crystal StructureHide

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IDSpeciesReferenceLinkYearLocalityPressure (GPa)Temp (K)
0007100YazganiteSarp H, Cerny R (2005) Yazganite, NaFe3+2(Mg,Mn)(AsO4)3*H2O, a new mineral: its description and crystal structure European Journal of Mineralogy 17 367-3732005Volcanic complex of Erciyes, Kiranardi, Turkey0293
CIF Raw Data - click here to close

X-Ray Powder DiffractionHide

Powder Diffraction Data:
d-spacingIntensity
6.40 Å(20)
5.63 Å(20)
3.575 Å(30)
3.202 Å(40)
2.917 Å(35)
2.768 Å(100)
2.611 Å(40)
Comments:
From type description.

Geological EnvironmentHide

Paragenetic Mode(s):
Paragenetic ModeEarliest Age (Ga)
Stage 7: Great Oxidation Event<2.4
46 : Near-surface hydrothermal alteration of minerals (see also #22)

Type Occurrence of YazganiteHide

General Appearance of Type Material:
Isolated prismatic crystals or aggregates formed by intergrown perfect crystals to 10x3x2 mm maximum size.
Place of Conservation of Type Material:
Department of Mineralogy, Natural History Museum of Geneva, Switzerland, 478.188.
Geological Setting of Type Material:
In andesitic rocks of the volcanic complex of Erciyes.
Associated Minerals at Type Locality:

Synonyms of YazganiteHide

Other Language Names for YazganiteHide

Dutch:Yazganiet
German:Yazganit
Simplified Chinese:水砷镁钠高铁石
Traditional Chinese:水砷鎂鈉高鐵石

Relationship of Yazganite to other SpeciesHide

Other Members of Alluaudite Group:
Alluaudite(Na,Ca)Mn2+(Fe3+,Mn2+,Fe2+,Mg)2(PO4)3Mon. 2/m : B2/b
'Alluaudite-Ca[]'◻4Ca4Mn2+4Fe3+8(PO4)12Mon. 2/m : B2/b
'Alluaudite-Na[]'◻4Na4Mn2+4Fe3+8(PO4)12Mon. 2/m : B2/b
ArseniopleiteNaCaMnMn2(AsO4)3Mon. 2/m
BadaloviteNa2Mg2Fe(AsO4)3Mon. 2/m : B2/b
BradaczekiteNaCu4(AsO4)3Mon. 2/m : B2/b
CalciohatertiteNaNaCa(CaFe3+)(AsO4)3Mon. 2/m : B2/b
CalciojohilleriteNaCaMg3(AsO4)3Mon. 2/m : B2/b
CamanchacaiteNaCaMg2[AsO4][AsO3(OH)]2Mon. 2/m : B2/b
CanutiteNaMn3[AsO4][AsO3(OH)]2Mon. 2/m : B2/b
Caryinite(Na,Pb)(Ca,Na)CaMn2+2(AsO4)3Mon. 2/m
ErikapohliteCu3(Zn,Cu,Mg)4Ca2(AsO4)6 · 2H2OMon. 2/m : B2/m
Ferroalluaudite(Na,Ca)Fe2+(Fe3+,Mn2+,Fe2+)2(PO4)3Mon. 2/m : B2/b
'Ferroalluaudite-NaNa'Na4Na4Fe2+4Fe3+8(PO4)12Mon. 2/m : B2/m
'Ferrohagendorfite'NaCaFe2+Fe2+2(PO4)3Mon.
GroatiteNaCaMn2(PO4)[PO3(OH)]2Mon. 2/m : B2/b
HagendorfiteNaCaMn2+Fe2+2(PO4)3Mon. 2/m : B2/b
'Hagendorfite-NaNa'NaNaFe2+(Mn2+,Mn3+)(PO4)3 (?)Mon. 2/m : B2/b
HatertiteNa2(Ca,Na)(Fe3+,Cu)2(AsO4)3Mon. 2/m : B2/b
JohilleriteNa(Mg,Zn)3Cu(AsO4)3Mon. 2/m : B2/b
KeyiteCu2+3Zn4Cd2(AsO4)6 · 2H2OMon. 2/m
KhrenoviteNa3Fe3+2(AsO4)3Mon. 2/m : B2/b
Maghagendorfite(Na,◻)MgMn2+(Fe2+,Fe3+)2(PO4)3Mon. 2/m
MagnesiocanutiteNaMnMg2[AsO4]2[AsO2(OH)2]Mon. 2/m : B2/b
Magnesiohatertite(Na,Ca)2Ca(Mg,Fe3+)2(AsO4)3Mon. 2/m : B2/b
NickenichiteNa0.8Ca0.4Cu0.4(Mg,Fe)3(AsO4)3Mon. 2/m : B2/b
O'DanieliteNa(Zn,Mg)3(AsO4)(AsO3OH)2Mon. 2/m : B2/b
ParaberzeliiteNaCa2Mg2(AsO4)3Mon. 2/m : B2/b
'Unnamed (Mn-analogue of Alluaudite)'(Na,Ca)Mn2+(Mn3+,Fe3+,Fe2+)2(PO4)3
'Unnamed (Na-Mg Arsenate Hydroxyarsenate)'NaMg3(AsO4)(AsO3OH)2Mon. 2/m : B2/b
'Unnamed (Na-Zn-H Arsenate Hydroxyarsenate)'Na(Na0.6Zn0.4)Zn2(H0.6AsO4)(AsO3OH)2Mon. 2/m : B2/b
VaruliteNaCaMn2+Mn2+2(PO4)3Mon. 2/m : B2/b
ZhanghuifeniteNa3Mn4Mg2Al(PO4)6Mon. 2/m
ZincobradaczekiteNaZn2Cu2(AsO4)3Mon. 2/m : B2/b

Related Minerals - Strunz-mindat GroupingHide

8.CF.FerraioloiteMgMn2+4(Fe2+0.5Al3+0.5)4Zn4(PO4)8(OH)4(H2O)20Mon.
8.CF.NaalasiteNaAl(AsO3OH)2 · H2OTrig. 32 : R32
8.CF.NafeasiteNa3Fe3+3(AsO3OH)6 · 3H2OMon. 2 : B2
8.CF.FalsteriteCa2MgMn2+2Fe2+2Fe3+2Zn4(PO4)8(OH)4(H2O)14Mon. 2/m : P21/b
8.CF.EspadaiteNa4Ca3Mg2[AsO3(OH)]2[AsO2(OH)2]10 · 7H2OOrth. mmm(2/m2/m2/m) : Ccca
8.CF.LiraiteNaCa2Mn2+2[Fe3+Fe2+]Mn2+2(PO4)6(H2O)2Orth. mm2
8.CF.05Tassieite(Na,◻)Ca2(Mg,Fe2+,Fe3+)2(Fe2+,Mg)2(Fe3+,Mg)2(PO4)6 · 2H2OOrth. mmm(2/m2/m2/m) : Pbca
8.CF.05BederiteCa2(Mn2+)4(Fe3+)2(PO4)6 · 2H2OOrth. mmm(2/m2/m2/m)
8.CF.05WicksiteNaCa2(Fe2+,Mn2+)4MgFe3+(PO4)6 · 2H2OOrth. mmm(2/m2/m2/m) : Pbca
8.CF.05GrischuniteNaCa2Mn2+5Fe3+(AsO4)6 · 2H2OOrth. mmm(2/m2/m2/m)
8.CF.05Maneckiite(Na◻)Ca2Fe2+2(Fe3+Mg)Mn2(PO4)6 · 2H2OOrth. mmm(2/m2/m2/m) : Pbca
8.CF.10HaigerachiteKFe3+3(PO3OH)2[PO2(OH)2]6 · 4H2OMon. 2/m : B2/b
8.CF.15CurrieriteNa4Ca3MgAl4(AsO3OH)12 · 9H2OHex. 622 : P622
8.CF.20RíosecoiteCa2Mg(AsO3OH)3(H2O)2Tric. 1 : P1

Other InformationHide

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 YazganiteHide

References for YazganiteHide

Localities for YazganiteHide

Showing 1 localities.

ⓘ - 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.
Turkey (TL)
 
  • Kayseri Province
    • Talas District
      • Kiranardi
        • Kültepe
          • Hisarcık
Sarp et al. (2005)
 
and/or  
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