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Martyite

A valid IMA mineral species
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About MartyiteHide

03665740014947997743512.jpg
Joe Marty
Formula:
Zn3(V2O7)(OH)2 · 2H2O
Colour:
pale orange yellow
Lustre:
Adamantine
Hardness:
3
Specific Gravity:
3.37
Crystal System:
Trigonal
Name:
Named for Mr. Joe Marty (1945- ), American medical technologist and mineral collector/micromounter, a member of the micromounters hall of fame, in recognition for his contributions to mineralogy.
Zn analogue of volborthite and karpenkoite.


Unique IdentifiersHide

Mindat ID:
32207
Long-form identifier:
mindat:1:1:32207:8
GUID
(UUID V4):
91a295d7-6472-4695-a8af-ced94405659c

IMA Classification of MartyiteHide

Approved
IMA Formula:
Zn3V2O7(OH)2 · 2H2O
Approval year:
2007

Classification of MartyiteHide

8.FD.05

8 : PHOSPHATES, ARSENATES, VANADATES
F : Polyphosphates, Polyarsenates, [4]-Polyvanadates
D : Polyphosphates, etc., with OH and H2O
40.3.10.2

40 : HYDRATED NORMAL PHOSPHATES,ARSENATES AND VANADATES
3 : A3(XO4)2·xH2O

Mineral SymbolsHide

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

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

Physical Properties of MartyiteHide

Adamantine
Transparency:
Transparent
Colour:
pale orange yellow
Hardness:
Tenacity:
Flexible
Cleavage:
Perfect
perfect on {001} and good on {110}
Comment:
thin flakes slightly flexible, coarser plates brittle with a curved fracture
Density:
3.37(3) g/cm3 (Measured)    3.375 g/cm3 (Calculated)

Optical Data of MartyiteHide

Type:
Uniaxial (+)
RI values:
nω = 1.793(3) nε = 1.806(3)
Max Birefringence:
δ = 0.013
Image shows birefringence interference colour range (at 30µm thickness)
and does not take into account mineral colouration.
Surface Relief:
Very High
Pleochroism:
Strong
Comments:
O (red-orange) >> E (yellow)

Chemistry of MartyiteHide

Mindat Formula:
Zn3(V2O7)(OH)2 · 2H2O

Crystallography of MartyiteHide

Crystal System:
Trigonal
Class (H-M):
3m - Ditrigonal Pyramidal
Space Group:
P3m1
Cell Parameters:
a = 6.0818 Å, c = 7.1793 Å
Ratio:
a:c = 1 : 1.18
Unit Cell V:
229.97 ų
Z:
1
Morphology:
thin plates and flakes with {001} prominent. A poorly developed {110} also observed.

Crystal StructureHide

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IDSpeciesReferenceLinkYearLocalityPressure (GPa)Temp (K)
0006193MartyiteKampf A R, Steele I M (2008) Martyite, a new mineral species related to volborthite: Description and crystal structure The Canadian Mineralogist 46 687-6922008Blue Cap mine, San Juan County, Utah0293
CIF Raw Data - click here to close

X-Ray Powder DiffractionHide

Powder Diffraction Data:
d-spacingIntensity
7.211 Å(100)
4.252 Å(20)
2.968 Å(50)
2.628 Å(35)
2.470 Å(40)
1.773 Å(20)
1.513 Å(20)
1.485 Å(25)

Geological EnvironmentHide

Paragenetic Mode(s):
Paragenetic ModeEarliest Age (Ga)
Stage 7: Great Oxidation Event<2.4
47a : [Near-surface hydration of prior minerals]
47e : [Vanadates, chromates, manganates]

Type Occurrence of MartyiteHide

General Appearance of Type Material:
a V-U oxide-replacement assemblage developed at the expense of organic material.
Place of Conservation of Type Material:
Natural History Museum of Los Angeles County, California, USA (catalog numbers 58610 and 58611).
Associated Minerals at Type Locality:

Synonyms of MartyiteHide

Other Language Names for MartyiteHide

Simplified Chinese:水钒锌石

Relationship of Martyite to other SpeciesHide

Other Members of this group:
KarpenkoiteCo3(V2O7)(OH)2 · 2H2OTrig. 3m (3 2/m) : P3m1
VolborthiteCu3(V2O7)(OH)2 · 2H2OMon. 2/m : B2/m

Common AssociatesHide

Associated Minerals Based on Photo Data:
1 photo of Martyite associated with CalciteCaCO3

Related Minerals - Strunz-mindat GroupingHide

8.FD.05VolborthiteCu3(V2O7)(OH)2 · 2H2OMon. 2/m : B2/m
8.FD.05KarpenkoiteCo3(V2O7)(OH)2 · 2H2OTrig. 3m (3 2/m) : P3m1
8.FD.10VanarsiteNaCa12(As3+V5+8.5V4+3.5As5+6O51)2 · 78H2OMon. 2/m : P21/b
8.FD.10PackratiteCa11(As3+V5+10V4+2As5+6O51)2 · 83H2OTric. 1 : P1
8.FD.10MorrisoniteCa11(As3+V4+2V5+10As5+6O51)2 · 78H2OMon. 2/m : P21/b
8.FD.10GatewayiteCa6(As3+V4+3 V5+9As5+6O51) · 31H2OMon. 2 : P21
8.FD.10KegginitePb3Ca3[AsV12O40(VO)] · 20H2OTrig. 3 : P3
8.FD.10Bicapite[KNa2Mg2(H2O)25][H2PV5+12O40(V5+O)2]Tet. 4/m : I4/m
8.FD.10LumsdeniteNaCa3Mg2(As3+V4+2V5+10As5+6O51) · 45H2OTric. 1 : P1
8.FD.15ChinchorroiteNa2Mg5(As2O7)2(AsO3OH)2(H2O)10Tric. 1 : P1

Other InformationHide

Notes:
Dissolves rapidly in cold 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 MartyiteHide

References for MartyiteHide

Localities for MartyiteHide

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.

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.
USA
 
  • Colorado
    • Mesa County
      • Gateway Mining District
        • Beaver Mesa
Kampf et al. (2017)
    • San Miguel County
      • Slick Rock Mining District
Collection Stephan Wolfsried +1 other reference
  • Utah
    • Grand County
      • Thompsons Mining District
        • Yellow Cat Mesa
Kasatkin et al. (2014) +1 other reference
    • San Juan County
      • La Sal Creek Mining District
Kampf et al. (2008) +1 other reference
Kampf et al. (2012)
 
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