Zincostrunzite
A valid IMA mineral species
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About Zincostrunzite
Formula:
ZnFe3+2(PO4)2(OH)2 · 6.5H2O
Colour:
Light brownish yellow; silvery white
Lustre:
Vitreous, Silky
Hardness:
2½
Specific Gravity:
2.66
Crystal System:
Triclinic
Member of:
Chemically related to steinmetzite, zincoberaunite, and UM2006-27-PO:FeHZn, the latter being a lower hydrate equivalent of the species. Also chemically similar to plimerite, wilhelmgümbelite, zinclipscombite, and phosphophyllite.
Unique Identifiers
Mindat ID:
47921
Long-form identifier:
mindat:1:1:47921:5
GUID
(UUID V4):
(UUID V4):
98d692ef-5609-46fa-9ae6-ee2fc0f84dc0
IMA Classification of Zincostrunzite
Approved
Approval year:
2016
First published:
2017
Type description reference:
Kampf, Anthony R., Grey, Ian E., Alves, Pedro, Mills, Stuart J., Nash, Barbara P., MaCrae, Colin M., Keck, Erich (2017) Zincostrunzite, ZnFe3+2(PO4)2(OH)2 · 6.5H2O, a new mineral from the Sitio do Castelo mine, Portugal, and the Hagendorf-Süd pegmatite, Germany. European Journal of Mineralogy, 29 (2) 315-322 doi:10.1127/ejm/2017/0029-2593
Classification of Zincostrunzite
8.DC.25
8 : PHOSPHATES, ARSENATES, VANADATES
D : Phosphates, etc. with additional anions, with H2O
C : With only medium-sized cations, (OH, etc.):RO4 = 1:1 and < 2:1
8 : PHOSPHATES, ARSENATES, VANADATES
D : Phosphates, etc. with additional anions, with H2O
C : With only medium-sized cations, (OH, etc.):RO4 = 1:1 and < 2:1
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 |
---|---|---|
Zstz | 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 Zincostrunzite
Vitreous, Silky
Colour:
Light brownish yellow; silvery white
Streak:
White
Hardness:
2½ on Mohs scale
Tenacity:
Brittle
Cleavage:
Perfect
At least one perfect cleavage parallel to [001]; probably either {1−10} or {100}
At least one perfect cleavage parallel to [001]; probably either {1−10} or {100}
Fracture:
Splintery
Density:
2.66 g/cm3 (Measured)
Optical Data of Zincostrunzite
Type:
Biaxial (-)
RI values:
nα = 1.620(2) nβ = 1.672(2) nγ = 1.720(2)
2V:
Measured: 89.5° (5), Calculated: 85.1°
Max Birefringence:
δ = 0.100
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:
High
Pleochroism:
Visible
Comments:
X nearly colourless, Y light brownish yellow, Z darker brownish yellow (X< Y< Z).
Chemistry of Zincostrunzite
Mindat Formula:
ZnFe3+2(PO4)2(OH)2 · 6.5H2O
Chemical Analysis
Empirical formulas:
Sample ID | Empirical Formula |
---|---|
1 | (Zn0.74Mn2+0.23)Σ 0.97Fe3+1.99(PO4)2(OH)2·6.5H2O |
2 | (Zn0.93Mn2+0.08)Σ1.01(Fe3+1.84Mn2+0.19)Σ2.03(PO4)2(OH)2·6.5H2O |
Sample references:
Crystallography of Zincostrunzite
Crystal System:
Triclinic
Class (H-M):
1 - Pinacoidal
Space Group:
P1
Cell Parameters:
a = 10.1736(6) Å, b = 9.7999(5) Å, c = 7.3296(2) Å
α = 91.325(4)°, β = 97.895(6)°, γ = 116.948(4)°
α = 91.325(4)°, β = 97.895(6)°, γ = 116.948(4)°
Ratio:
a:b:c = 1.038 : 1 : 0.748
Unit Cell V:
642.22 ų
Z:
2
Morphology:
Elongated on [001] with the prism forms {010} and {1−10} and poorly formed terminations, probably {001}.
Twinning:
Twinning is ubiquitous by 180° rotation on [0 1 0] with the composition plane {1−20}
X-Ray Powder Diffraction
Powder Diffraction Data:
d-spacing | Intensity |
---|---|
8.87 Å | (100) |
5.32 Å | (95) |
4.457 Å | (30) |
4.287 Å | (41) |
3.310 Å | (29) |
3.220 Å | (75) |
1.912 Å | (25) |
1.622 Å | (32) |
Geological Environment
Paragenetic Mode(s):
Paragenetic Mode | Earliest Age (Ga) |
---|---|
Stage 4b: Highly evolved igneous rocks | >3.0 |
34 : Complex granite pegmatites | |
Stage 7: Great Oxidation Event | <2.4 |
47a : [Near-surface hydration of prior minerals] | |
47c : [Carbonates, phosphates, borates, nitrates] |
Type Occurrence of Zincostrunzite
Co-Type Localities:
General Appearance of Type Material:
Sitio do Castelo: as prisms up to 2 mm long
Hagendorf: the mineral makes up portions of needles that are up to about 5 mm long.
Hagendorf: the mineral makes up portions of needles that are up to about 5 mm long.
Place of Conservation of Type Material:
Cotype material is deposited in the collections of the Mineral Sciences Department, Natural History Museum of Los Angeles County, 900 Exposition Boulevard, Los Angeles, California 90007, USA, catalogue numbers 65646 and 65647 (Sitio do Castelo), and the
Empirical Formula of Type Material:
(Zn0.93Mn2+0.08)Σ1.01(Fe3+1.84Mn2+0.19)Σ2.03(PO4)2(OH)2·6.5H2O
Geological Setting of Type Material:
Pegmatite
Reference:
Kampf, A.R., Grey, I.E., Alves, P., Mills, S.J., Nash, B.P., MacRae, C.M., Keck, E. (2017): Zincostrunzite, ZnFe3+2(PO4)2(OH)2.6.5H2O, a new mineral from the Sitio do Castelo mine, Portugal, and the Hagendorf-Sud pegmatite, Germany. European Journal of Mineralogy, 29, 315-322.
Synonyms of Zincostrunzite
Relationship of Zincostrunzite to other Species
Member of:
Other Members of this group:
Ferristrunzite | Fe3+Fe3+2(PO4)2(OH)3 · 5H2O | Tric. |
Ferrostrunzite | Fe2+Fe3+2(PO4)2(OH)2 · 6H2O | Tric. |
Strunzite | Mn2+Fe3+2(PO4)2(OH)2 · 6H2O | Tric. 1 : P1 |
Common Associates
Associated Minerals Based on Photo Data:
Related Minerals - Strunz-mindat Grouping
8.DC. | Ianbruceite | Zn2(AsO4)(OH) · 3H2O |
8.DC. | Césarferreiraite | Fe2+ Fe3+2(AsO4)2(OH)2 · 8H2O |
8.DC. | Ferrivauxite | Fe3+Al2(PO4)2(OH)3 · 5H2O |
8.DC.05 | Nissonite | Cu2Mg2(PO4)2(OH)2 · 5H2O |
8.DC.07 | Euchroite | Cu2(AsO4)(OH) · 3H2O |
8.DC.10 | Legrandite | Zn2(AsO4)(OH) · H2O |
8.DC.12 | Strashimirite | Cu8(AsO4)4(OH)4 · 5H2O |
8.DC.15 | Arthurite | CuFe3+2(AsO4)2(OH)2 · 4H2O |
8.DC.15 | Earlshannonite | Mn2+Fe3+2(PO4)2(OH)2 · 4H2O |
8.DC.15 | Ojuelaite | ZnFe3+2(AsO4)2(OH)2 · 4H2O |
8.DC.15 | Whitmoreite | Fe2+Fe3+2(PO4)2(OH)2 · 4H2O |
8.DC.15 | Cobaltarthurite | (Co,Mg)Fe3+2(AsO4)2(OH)2 · 4H2O |
8.DC.15 | Bendadaite | Fe2+Fe3+2(AsO4)2(OH)2 · 4H2O |
8.DC.15 | Kunatite | CuFe3+2(PO4)2(OH)2 · 4H2O |
8.DC.15 | UM2006-27-PO:FeHZn | ZnFe3+2(PO4)2(OH)2 · 4H2O |
8.DC.15 | UKI-2006-(PO:AlCuFeH) | Fe2+Al3+2(PO4)2(OH)2 · 4H2O |
8.DC.17 | Kleemanite | ZnAl2(PO4)2(OH)2 · 3H2O |
8.DC.20 | Bermanite | Mn2+Mn3+2(PO4)2(OH)2 · 4H2O |
8.DC.20 | Coralloite | Mn2+Mn3+2(AsO4)2(OH)2 · 4H2O |
8.DC.20 | Magnesiobermanite | MgMn3+2(PO4)2(OH)2 · 4H2O |
8.DC.22 | Kovdorskite | Mg2(PO4)(OH) · 3H2O |
8.DC.25 | Ferristrunzite | Fe3+Fe3+2(PO4)2(OH)3 · 5H2O |
8.DC.25 | Ferrostrunzite | Fe2+Fe3+2(PO4)2(OH)2 · 6H2O |
8.DC.25 | Metavauxite | Fe2+Al2(PO4)2(OH)2 · 8H2O |
8.DC.25 | Metavivianite | Fe2+Fe3+2(PO4)2(OH)2 · 6H2O |
8.DC.25 | Strunzite | Mn2+Fe3+2(PO4)2(OH)2 · 6H2O |
8.DC.27 | Beraunite | Fe3+6(PO4)4O(OH)4 · 6H2O |
8.DC.27 | Tvrdýite | Fe2+Fe3+2 Al3(PO4)4(OH)5(H2O)4 · 2H2O |
8.DC.27 | Zincoberaunite | ZnFe3+5(PO4)4(OH)5 · 6H2O |
8.DC.30 | Gordonite | MgAl2(PO4)2(OH)2 · 8H2O |
8.DC.30 | Laueite | Mn2+Fe3+2(PO4)2(OH)2 · 8H2O |
8.DC.30 | Mangangordonite | Mn2+Al2(PO4)2(OH)2 · 8H2O |
8.DC.30 | Paravauxite | Fe2+Al2(PO4)2(OH)2 · 8H2O |
8.DC.30 | Pseudolaueite | Mn2+Fe3+2(PO4)2(OH)2 · 8H2O |
8.DC.30 | Sigloite | Fe3+Al2(PO4)2(OH)3 · 7H2O |
8.DC.30 | Stewartite | Mn2+Fe3+2(PO4)2(OH)2 · 8H2O |
8.DC.30 | Ushkovite | MgFe3+2(PO4)2(OH)2 · 8H2O |
8.DC.30 | Ferrolaueite | Fe2+Fe3+2(PO4)2(OH)2 · 8H2O |
8.DC.30 | Kastningite | (Mn2+,Fe2+,Mg)Al2(PO4)2(OH)2 · 8H2O |
8.DC.30 | Maghrebite | MgAl2(AsO4)2(OH)2 · 8H2O |
8.DC.30 | Nordgauite | MnAl2(PO4)2(F,OH)2 · 5H2O |
8.DC.30 | Kayrobertsonite | [MnAl2(PO4)2(OH)2(H2O)4] · 2H2O |
8.DC.30 | Kummerite | Mn2+Fe3+Al(PO4)2(OH)2 · 8H2O |
8.DC.32 | Tinticite | Fe3+3(PO4)2(OH)3 · 3H2O |
8.DC.32 | Kamarizaite | Fe3+3(AsO4)2(OH)3 · 3H2O |
8.DC.35 | Vauxite | Fe2+Al2(PO4)2(OH)2 · 6H2O |
8.DC.37 | Vantasselite | Al4(PO4)3(OH)3 · 9H2O |
8.DC.40 | Cacoxenite | Fe3+24AlO6(PO4)17(OH)12 · 75H2O |
8.DC.45 | Gormanite | (Fe2+,Mg)3(Al,Fe3+)4(PO4)4(OH)6 · 2H2O |
8.DC.45 | Souzalite | (Mg,Fe2+)3(Al,Fe3+)4(PO4)4(OH)6 · 2H2O |
8.DC.47 | Kingite | Al3(PO4)2F2(OH) · 7H2O |
8.DC.50 | Wavellite | Al3(PO4)2(OH,F)3 · 5H2O |
8.DC.50 | Allanpringite | Fe3+3(PO4)2(OH)3 · 5H2O |
8.DC.50 | Fluorwavellite | Al3(PO4)2(OH)2F · 5H2O |
8.DC.52 | Kribergite | Al5(PO4)3(SO4)(OH)4 · 4H2O |
8.DC.55 | Mapimite | Zn2Fe3+3(AsO4)3(OH)4 · 10H2O |
8.DC.57 | Ogdensburgite | Ca2Fe3+4(Zn,Mn2+)(AsO4)4(OH)6 · 6H2O |
8.DC.60 | Nevadaite | (Cu2+,Al,V3+)6Al8(PO4)8F8(OH)2 · 22H2O |
8.DC.60 | Cloncurryite | Cu0.5(VO)0.5Al2(PO4)2F2 · 5H2O |
8.DC.62 | Kenngottite | Mn2+3Fe3+4(PO4)4(OH)6(H2O)2 |
8.DC.67 | Molinelloite | Cu(H2O)(OH)V4+O(V5+O4) |
8.DC.70 | Whitecapsite | H16Fe2+5Fe3+14Sb3+6(AsO4)18O16 · 120H2O |
8.DC.75 | Heimite | PbCu2(AsO4)(OH)3 · 2H2O |
8.DC.80 | Lednevite | Cu[PO3(OH)] · H2O |
Other Information
Notes:
At room temperature, the mineral is slowly soluble in dilute HCl and rapidly 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 Zincostrunzite
mindat.org URL:
https://www.mindat.org/min-47921.html
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References for Zincostrunzite
Reference List:
Hålenius, U., Hatert, F., Pasero, M., Mills, S. J. (2016) New minerals and nomenclature modifications approved in 2016, CNMNC Newsletter 32. Mineralogical Magazine, 80 (5) 915-922 doi:10.1180/minmag.2016.080.084
Kampf, Anthony R., Grey, Ian E., Alves, Pedro, Mills, Stuart J., Nash, Barbara P., MaCrae, Colin M., Keck, Erich (2017) Zincostrunzite, ZnFe3+2(PO4)2(OH)2 · 6.5H2O, a new mineral from the Sitio do Castelo mine, Portugal, and the Hagendorf-Süd pegmatite, Germany. European Journal of Mineralogy, 29 (2) 315-322 doi:10.1127/ejm/2017/0029-2593
Localities for Zincostrunzite
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.
Germany (TL) | |
| Mineralogical Magazine +2 other references |
Portugal (TL) | |
| Mineralogical Magazine +2 other references |
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Sítio do Castelo Mine, Folgosinho, Gouveia, Guarda, Portugal