Sincosite (original) (raw)
A valid IMA mineral species - grandfathered
About SincositeHide
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Formula:
Ca(VO)2(PO4)2 · 5H2O
Colour:
Grass-green, yellow- to olive-green, brownish green, blue-green; light green, olive-green, brownish green, yellowish green, bluish green in transmitted light.
Lustre:
Vitreous, Pearly, Sub-Metallic, Dull
Specific Gravity:
2.84 - 2.98
Crystal System:
Tetragonal
Name:
Named after its discovery locality at Sincos, Junín, Cerro de Pasco, Alcides Carrión Province, Pasco Department, Peru.
Unique IdentifiersHide
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Long-form identifier:
mindat:1:1:3671:5
cf6a8217-d55e-4760-b530-73d79381cfff
IMA Classification of SincositeHide
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Approved, 'Grandfathered' (first described prior to 1959)
IMA Formula:
Ca(VO)2(PO4)2 · 4H2O
Type description reference:
Classification of SincositeHide
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8.CJ.65
8 : PHOSPHATES, ARSENATES, VANADATES
C : Phosphates without additional anions, with H2O
J : With only large cations
42.11.19.1
42 : HYDRATED PHOSPHATES, ETC.CONTAINING HYDROXYL OR HALOGEN
11 : (AB)3(XO4)2Zq·xH2O
19.10.10
19 : Phosphates
10 : Phosphates of Pb, Th, V and Bi
Mineral SymbolsHide
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As of 2021 there are now IMA–CNMNC approved mineral symbols (abbreviations) for each mineral species, useful for tables and diagrams.
Symbol | Source | Reference |
---|---|---|
Scs | 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 SincositeHide
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Vitreous, Pearly, Sub-Metallic, Dull
Transparency:
Transparent, Translucent
Comment:
Lustre pearly on basal cleavage; submetallic if partially dehydrated
Colour:
Grass-green, yellow- to olive-green, brownish green, blue-green; light green, olive-green, brownish green, yellowish green, bluish green in transmitted light.
Comment:
Typically zoned parallel to {001}.
Cleavage:
Perfect
On (001) perfect, on {110} good, on {010} poor.
Density:
2.84 - 2.98 g/cm3 (Measured) 2.97 g/cm3 (Calculated)
Comment:
Actual value for measured density is ~2.84 to 2.98.
Optical Data of SincositeHide
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RI values:
_n_α = 1.670 - 1.675 _n_β = 1.690 _n_γ = 1.693 - 1.694 _n_ω = 1.680 _n_ε = 1.655
δ = 0.025
Image shows birefringence interference colour range (at 30µm thickness)
and does not take into account mineral colouration.
Comments:
E = X = Nearly colourless to pale yellow
O = Z = Grey-green
Comments:
Partially biaxial (-) if dehydrated.
Chemistry of SincositeHide
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Mindat Formula:
Ca(VO)2(PO4)2 · 5H2O
Crystallography of SincositeHide
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Polytype:
Formula:
Crystal System:
Class (H-M)
Space Group:
Space Group Setting:
Cell Parameters:
Ratio:
Unit Cell Volume (calc):
Z:
Sincosite (triclinic polytype) |
---|
Triclinic |
1 - Pedial |
_P_1 |
a = 6.3531(12) Å, b = 6.3567(14) Å, c = 6.6050(18) Åα = 106.995(22)°, β = 94.115(19)°, γ = 90.006(16)° |
a:b:c = 0.999 : 1 : 1.039 |
V 254.37 ų(Calculated from Unit Cell) |
Crystal StructureHide
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ID | Species | Reference | Link | Year | Locality | Pressure (GPa) | Temp (K) |
---|---|---|---|---|---|---|---|
0012705 | Sincosite | Kang H Y, Lee W C, Wang S L (1992) Hydrothermal synthesis and structural characterization of four layered vanadyl(IV) phosphate hydrates A(VO)2(PO4)2*4H2O (A=Co,Ca,Sr,Pb) Inorganic Chemistry 31 4743-4748 | 1992 | synthetic | 0 | 293 | |
0015719 | Sincosite | Franke W A, Luger P, Weber M, Ivanova T I (1997) Low hydrothermal growth of sincosite Ca(VO/PO4)2*4H2O Zapiski Vserossijskogo Mineralogicheskogo Obshchestva 126N2 85-86 | 1997 | synthetic | 0 | 293 |
CIF Raw Data - click here to close
X-Ray Powder DiffractionHide
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Powder Diffraction Data:
d-spacing | Intensity |
---|---|
6.35 Å | (100) |
3.190 Å | (80) |
3.511 Å | (60) |
2.682 Å | (50) |
2.907 Å | (40) |
2.100 Å | (40) |
3.841 Å | (25) |
Geological EnvironmentHide
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Type Occurrence of SincositeHide
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Place of Conservation of Type Material:
National School of Mines, Paris, France. Harvard University, Cambridge, Massachusetts, USA: #99139, 101699. U.S. National Museum of Natural History, Washington, D.C., USA: #95096.
Geological Setting of Type Material:
Veinlets in Cretaceous black carbonaceous shale
Associated Minerals at Type Locality:
Reference:
Schaller, W.T. (1922) Sincosite, a new mineral. Journal of the Washington Academy of Sciences: 12: 195-195.
Other Language Names for SincositeHide
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Common AssociatesHide
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Associated Minerals Based on Photo Data:
Related Minerals - Strunz-mindat GroupingHide
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8.CJ. | Sainfeldite | Ca5(AsO4)2(AsO3OH)2 · 4H2O | Mon. 2/m : _B_2/b |
---|---|---|---|
8.CJ. | Caesiumpharmacosiderite | CsFe4[(AsO4)3(OH)4] · 4H2O | Iso. 43_m_ : P_43_m |
8.CJ. | Jeankempite | Ca5(AsO4)2(HAsO4)2 · 7H2O | Tric. 1 : _P_1 |
8.CJ. | Airdite | Sr(V4+O)2(PO4)2 · 4H2O | Mon. m : B b |
8.CJ. | Dobšináite | Ca2Ca(AsO4)2 · 2H2O | Mon. 2/m : _P_21/b |
8.CJ.05 | Stercorite | (NH4)Na(PO3OH) · 4H2O | Tric. 1 : _P_1 |
8.CJ.10 | Mundrabillaite | (NH4)2Ca(PO3OH)2 · H2O | Mon. m : P m |
8.CJ.10 | Swaknoite | (NH4)2Ca(PO3OH)2 · H2O | Orth. |
8.CJ.15 | Nabaphite | NaBaPO4 · 9H2O | Iso. 23 : _P_213 |
8.CJ.15 | Nastrophite | Na(Sr,Ba)PO4 · 9H2O | Iso. 23 : _P_213 |
8.CJ.20 | Haidingerite | CaHAsO4 · H2O | Orth. m m m _(_2/_m_2/_m_2/m ) : P b c n |
8.CJ.25 | Vladimirite | Ca4(AsO4)2(AsO3OH) · 4H2O | Mon. 2/m : _P_21/b |
8.CJ.25 | Rhabdophane-(Y) | YPO4 · H2O | Hex. 622 : _P_6222 |
8.CJ.27 | Churchite-(Dy) | (Dy,Sm,Gd,Nd)PO4 · 2H2O | Mon. |
8.CJ.30 | Ferrarisite | Ca5(AsO4)2(HAsO4)2 · 9H2O | Tric. 1 : _P_1 |
8.CJ.35 | Machatschkiite | (Ca,Na)6(AsO4)(HAsO4)3(PO4,SO4) · 15H2O | Trig. 3_m_ : R_3_c |
8.CJ.35 | Fulbrightite | Ca(VO)2(AsO4)2 · 4H2O | Tric. 1 : _P_1 |
8.CJ.40 | Phaunouxite | Ca3(AsO4)2 · 11H2O | Tric. |
8.CJ.40 | Rauenthalite | Ca3(AsO4)2 · 10H2O | Tric. 1 : _P_1 |
8.CJ.45 | Brockite | (Ca,Th,Ce)PO4 · H2O | Hex. 622 : _P_6222 |
8.CJ.45 | Grayite | (Th,Pb,Ca)(PO4) · H2O | Hex. 622 : _P_6222 |
8.CJ.45 | Rhabdophane-(Ce) | Ce(PO4) · 0.6H2O | Trig. 32 : _P_3121 |
8.CJ.45 | Rhabdophane-(La) | La(PO4) · H2O | Hex. 622 : _P_6222 |
8.CJ.45 | Rhabdophane-(Nd) | Nd(PO4) · H2O | Hex. 622 : _P_6222 |
8.CJ.45 | Tristramite | (Ca,U,Fe)(PO4,SO4) · 2H2O | Hex. 622 : _P_6222 |
8.CJ.45 | Smirnovskite | (Th,Ca)PO4 · nH2O | Hex. 622 : _P_6222 |
8.CJ.45 | Štěpite | U(AsO3OH)2 · 4H2O | Tet. 4/m m m _(_4/_m_2/_m_2/m ) : _I_41/a c d |
8.CJ.47 | Vysokýite | U4+[AsO2(OH)2]4 · 4H2O | Tric. 1 : _P_1 |
8.CJ.50 | Ardealite | Ca2(PO3OH)(SO4) · 4H2O | Mon. m : B b |
8.CJ.50 | Brushite | Ca(PO3OH) · 2H2O | Mon. m : B b |
8.CJ.50 | Churchite-(Y) | Y(PO4) · 2H2O | Mon. 2/m : _B_2/b |
8.CJ.50 | Pharmacolite | Ca(HAsO4) · 2H2O | Mon. m |
8.CJ.50 | Churchite-(Nd) | Nd(PO4) · 2H2O | Mon. |
8.CJ.55 | Mcnearite | NaCa5(AsO4)(HAsO4)4 · 4H2O | Tric. |
8.CJ.60 | Dorfmanite | Na2(PO3OH) · 2H2O | Orth. m m m _(_2/_m_2/_m_2/m ) : P b c a |
8.CJ.65 | Bariosincosite | Ba(VO)2(PO4)2 · 4H2O | Tet. |
8.CJ.70 | Catalanoite | Na2(PO3OH) · 8H2O | Orth. m m m _(_2/_m_2/_m_2/m ) : I b c a |
8.CJ.75 | Guérinite | Ca6(HAsO4)3(AsO4)2 · 10.5H2O | Mon. 2/m : _P_21/b |
8.CJ.85 | Ningyoite | (U,Ca,Ce)2(PO4)2 · 1-2H2O | Orth. |
Other InformationHide
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Notes:
Readily soluble in dilute acids to a blue solution. Insoluble in water.
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 SincositeHide
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References for SincositeHide
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Reference List:
Localities for SincositeHide
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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
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- 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.