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Mendozavilite-NaCu

A valid IMA mineral species
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About Mendozavilite-NaCuHide

Formula:
[Na2(H2O)15Cu(H2O)6][Mo8P2Fe3+3O34(OH)3]
Colour:
Lime green
Lustre:
Sub-Adamantine, Vitreous
Hardness:
Specific Gravity:
2.824
Crystal System:
Monoclinic
Name:
Named for the relationship to other mendozavilite group minerals and the dominant cations Na and Cu.
This page provides mineralogical data about Mendozavilite-NaCu.


Unique IdentifiersHide

Mindat ID:
41946
Long-form identifier:
mindat:1:1:41946:2

IMA Classification of Mendozavilite-NaCuHide

Classification of Mendozavilite-NaCuHide

7.GB.50

7 : SULFATES (selenates, tellurates, chromates, molybdates, wolframates)
G : Molybdates, Wolframates and Niobates
B : With additional anions and/or H2O

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

Physical Properties of Mendozavilite-NaCuHide

Sub-Adamantine, Vitreous
Transparency:
Transparent
Colour:
Lime green
Streak:
Colorless to very pale green
Hardness:
2½ on Mohs scale
Tenacity:
Flexible
Cleavage:
Perfect
{001}
Parting:
{001}
Fracture:
Irregular/Uneven
Density:
2.824(5) g/cm3 (Measured)    2.824 g/cm3 (Calculated)

Optical Data of Mendozavilite-NaCuHide

Type:
Biaxial (+)
RI values:
nα = 1.770(5) nβ = 1.785(5) nγ = 1.805(5)
2V:
Measured: 80° (10)
Max. Birefringence:
δ = 0.035
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.

Surface Relief:
Very High (positive)
Relative to Canada balsam mounting medium (n ≈ 1.537).

This shows the grain boundary and Becke line effect under plane-polarised light, based on the contrast between this mineral's average refractive index and the mounting medium. It does not take into account mineral colouration.
In focus
Interference Figure:
This shows the idealized biaxial acute bisectrix (Bxa) interference figure - the conoscopic view for a grain cut perpendicular to the acute bisectrix, using this mineral's 2V. The two small white dots mark the melatopes - the points where the two optic axes emerge - and are shown only when they fall within the field of view. The coloured bands are isochromatics, and the dark bands are isogyres.

Rotate the stage: at 0°/90° the isogyres form a cross through the melatopes; at 45° they pull apart into curved hyperbolas. That splitting on rotation - absent in a uniaxial figure - is the standard diagnostic test for telling biaxial minerals from uniaxial ones. If 2V is large, the melatopes may fall outside the field of view, as they often do at the microscope too.
Dispersion:
r < v, strong, inclined
Pleochroism:
Visible
Comments:
Pale olive green, Y > X = Z

Chemistry of Mendozavilite-NaCuHide

Mindat Formula:
[Na2(H2O)15Cu(H2O)6][Mo8P2Fe3+3O34(OH)3]
Element Weights:
Element% weight
O44.614 %
Mo36.908 %
Fe8.055 %
Cu3.055 %
P2.978 %
Na2.211 %
H2.181 %

Calculated from ideal end-member formula.
O
Mo
Fe
Cu
P
Na
H

Crystallography of Mendozavilite-NaCuHide

Crystal System:
Monoclinic
Class (H-M):
2/m - Prismatic
Space Group:
B2/m
Setting:
C2/m
Cell Parameters:
a = 18.9984(16) Å, b = 10.9296(7) Å, c = 15.0818(12) Å
β = 129.906(2)°
Ratio:
a:b:c = 1.738 : 1 : 1.38
Unit Cell V:
2,402.29 ų (Calculated from Unit Cell)
Morphology:
Sixsided (pseudohexagonal) tabular crystals up to 1 mm across and 0.1mm thick. Forms observed: {001},{110}, {111},{20-1} and {110}.
Twinning:
Ubiquitous: contact on {001} and penetration, both on roatation of 120° about [102].

X-Ray Powder DiffractionHide

Powder Diffraction Data:
d-spacingIntensity
8.841 Å(100)
7.330 Å(37)
3.676 Å(17)
3.132 Å(19)
3.007 Å(25)
2.932 Å(21)
2.743 Å(20)
1.769 Å(22)

Geological EnvironmentHide

Paragenetic Mode(s):
Paragenetic ModeEarliest Age (Ga)
Stage 7: Great Oxidation Event<2.4
47c : [Carbonates, phosphates, borates, nitrates]

Type Occurrence of Mendozavilite-NaCuHide

General Appearance of Type Material:
As thin vein fillings and well developed crystals in cavities of quartz
Place of Conservation of Type Material:
Natural History Museum of Los Angeles County, catalogue numbers 60483, 60484,60485 and 60486
Geological Setting of Type Material:
In the oxidation zone of a porphyry copper deposit
Associated Minerals at Type Locality:

Synonyms of Mendozavilite-NaCuHide

Other Language Names for Mendozavilite-NaCuHide

Relationship of Mendozavilite-NaCu to other SpeciesHide

Other Members of Mendozavilite Group:
Melkovite[Ca2(H2O)15Ca(H2O)6][Mo8P2Fe3+3O36(OH)]Mon. 2/m : B2/m
Mendozavilite-KCa[K2(H2O)15Ca(H2O)6][Mo8P2Fe3+3O34(OH)3] Mon. 2/m : B2/m
Mendozavilite-NaFe[Na2(H2O)15Fe3+(H2O)6][Mo8P2Fe3+3O35(OH)2]Mon. 2/m : B2/m

Related Minerals - Strunz-mindat GroupingHide

7.GB.Stunorthropite(NH4)4[Mo2O6(MoO4)2]Tric. 1 : P1
7.GB.HartkoppeiteCa4Mn2+Mo6+6As5+4O32(OH)2(H2O)14 · 5H2OTric. 1 : P1
7.GB.WangpuiteK3(PO4)(Mo12O36)Iso. m3m(4/m32/m) : Pn3m
7.GB.AlexearliteHg3S2(MoO4)Orth. mmm(2/m2/m2/m) : Pnma
7.GB.OotanniteTh4+2W6+4O16 · 5H2OMon. 2/m : P21/b
7.GB.NatromolybditeNa2MoO4 · 2H2OOrth. mmm(2/m2/m2/m) : Pbca
7.GB.Marsaalamite-(Y)Y(MoO4)(OH)Mon. 2/m : P21/b
7.GB.05LindgreniteCu3(MoO4)2(OH)2Mon. 2/m : P21/m
7.GB.10SzenicsiteCu3(MoO4)(OH)4Orth. mmm(2/m2/m2/m) : Pnnm
7.GB.15'UM1999-38-WO:CrV'(V, Cr, W, O, H) [V:Cr:W ratio about 2:1:3]
7.GB.15HueniteCu4(MoO4)3(OH)2Trig. 3m : P31c
7.GB.15CuprotungstiteCu2(WO4)(OH)2Tet. 422 : P41212
7.GB.20Phyllotungstite(H2O,M)x(W,Fe)(O,OH)3 · yH2O (M = Ca, Cs, Pb or K)Hex. 6/mmm(6/m2/m2/m) : P63/mmc
7.GB.25RankachiteCa0.5(V4+,V5+)(W6+,Fe3+)2O8(OH) · 2H2OMon. 2/m : P21/m
7.GB.30FerrimolybditeFe2(MoO4)3 · nH2OOrth. mmm(2/m2/m2/m) : Pmmn
7.GB.35MpororoiteWAlO3(OH)3 · 2(H2O)Tric.
7.GB.35AnthoiniteAlWO3(OH)3Tric. 1
7.GB.40Obradovicite-KCu[K2(H2O)17Cu(H2O)6][Mo8As2Fe3+3O34(OH)3]Orth. mmm(2/m2/m2/m) : Pmna
7.GB.45Paramendozavilite[KAl4(H2O)30][Mo12P6Fe3+6O60(OH)13]Mon.
7.GB.45Mendozavilite-NaFe[Na2(H2O)15Fe3+(H2O)6][Mo8P2Fe3+3O35(OH)2]Mon. 2/m : B2/m
7.GB.45Obradovicite-NaCuNa2(H2O)17Cu(H2O)6][Mo8As2Fe3+3O34(OH)3] Orth. mmm(2/m2/m2/m) : Pmna
7.GB.45Obradovicite-NaNa[Na2(H2O)16Na(H2O)6][Mo8As2Fe3+3O33(OH)4] Orth.
7.GB.50Tancaite-(Ce)FeCe(MoO4)3 · 3H2O Trig. 3 : R3
7.GB.50Mendozavilite-KCa[K2(H2O)15Ca(H2O)6][Mo8P2Fe3+3O34(OH)3] Mon. 2/m : B2/m
7.GB.60PeterandreseniteMn4Nb6O19 · 14H2OMon. 2/m : B2/m
7.GB.60HansesmarkiteCa2Mn2Nb6O19 · 20H2OTric. 1 : P1
7.GB.60MelcheriteBa2Na2Mg[Nb6O19] · 6H2OTrig. 3 : R3
7.GB.65IchnusaiteTh(MoO4)2 · 3H2OMon. 2/m : P21/b
7.GB.70MarkascheriteCu3(MoO4)(OH)4Mon. 2/m : P21/m
7.GB.75NuragheiteTh(MoO4)2 · H2OMon. 2/m : P21/b
7.GB.80OphiriteCa2Mg4[Zn2Mn3+2(H2O)2(Fe3+W9O34)2] · 46H2OTric. 1 : P1

Fluorescence of Mendozavilite-NaCuHide

Other InformationHide

Notes:
Slowly soluble in concentrated HCl
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 Mendozavilite-NaCuHide

References for Mendozavilite-NaCuHide

Localities for Mendozavilite-NaCuHide

Showing 2 localities.

This map shows a selection of localities that have latitude and longitude coordinates recorded. Click on the symbol to view information about a locality. The symbol next to localities in the list can be used to jump to that position on the map.
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Locality ListHide

- 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.
Chile (TL)
 
  • Antofagasta
    • Antofagasta Province
      • Sierra Gorda
        • Lomas Bayas mining district
Williams et al. (2011) +1 other reference
    • El Loa Province
      • Calama
        • Chuquicamata District
samples analysed by Tony Kampf
 
and/or  
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