Argandite (original) (raw)
A valid IMA mineral species
About ArganditeHide
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Crystal System:
Monoclinic
Name:
Named in honour of Emile Argand (1879-1940), Swiss geologist and mineralogist, who studied the tectonics of the Alps and of Asia. Argand was an early supporter of Wegener's theory of continental drift.
Unique IdentifiersHide
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Long-form identifier:
mindat:1:1:40277:2
0a4514af-8383-4390-87df-47631466e223
IMA Classification of ArganditeHide
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Classification of ArganditeHide
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8.BE.30
8 : PHOSPHATES, ARSENATES, VANADATES
B : Phosphates, etc., with additional anions, without H2O
E : With only medium-sized cations, (OH, etc.):RO4 > 2:1
41.2.1.4
41 : ANHYDROUS PHOSPHATES, ETC.CONTAINING HYDROXYL OR HALOGEN
2 : (AB)7(XO4)2Zq
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 |
---|---|---|
Agd | 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 ArganditeHide
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Cleavage:
Distinct/Good
Probably parallel to {001}.
Density:
3.71(5) g/cm3 (Measured) 3.67(1) g/cm3 (Calculated)
Optical Data of ArganditeHide
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RI values:
_n_α = 1.740 _n_β = 1.762(4) _n_γ = 1.770
δ = 0.030
Image shows birefringence interference colour range (at 30µm thickness)
and does not take into account mineral colouration.
Comments:
Orange-yellow to orange.
Chemistry of ArganditeHide
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Mindat Formula:
Mn7(VO4)2(OH)8
Crystallography of ArganditeHide
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Crystal System:
Monoclinic
Class (H-M):
2/m - Prismatic
Cell Parameters:
a = 5.498(2) Å, b = 12.265(3) Å, c = 10.092(2) Å
β = 95.594(3)°
Ratio:
a:b:c = 0.448 : 1 : 0.823
Unit Cell V:
677.29 ų (Calculated from Unit Cell)
Morphology:
Anhedral grains.
Crystal StructureHide
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ID | Species | Reference | Link | Year | Locality | Pressure (GPa) | Temp (K) |
---|---|---|---|---|---|---|---|
0018517 | Argandite | Brugger J, Elliott P, Meisser N, Ansermet S (2011) Argandite, Mn7(VO4)2(OH)8, the V analogue of allactite from the metamorphosed Mn ores at Pipji, Turtmann Valley, Switzerland American Mineralogist 96 1894-1900 | 2011 | Pipji, Turtmann Valley, Switzerland | 0 | 293 |
CIF Raw Data - click here to close
X-Ray Powder DiffractionHide
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Powder Diffraction Data:
d-spacing | Intensity |
---|---|
3.708 Å | (50) |
3.395 Å | (60) |
3.074 Å | (100) |
2.945 Å | (50) |
2.687 Å | (70) |
2.522 Å | (50) |
2.324 Å | (40) |
1.791 Å | (40) |
Comments:
Pipjitälli, Valais, Switzerland. The data are from the type description.
Geological EnvironmentHide
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Type Occurrence of ArganditeHide
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General Appearance of Type Material:
Argandite occurs as a rock-forming mineral in a manganosite-rich specimen. It forms orange anhedral grains up to 60 micron in diameter.
Place of Conservation of Type Material:
Geological Museum, Lausanne, Switzerland, reg. no. MGL90369.
Geological Setting of Type Material:
Metamorphosed synsedimentary exhalative Mn deposit.
Associated Minerals at Type Locality:
Synonyms of ArganditeHide
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Relationship of Argandite to other SpeciesHide
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Other Members of this group:
Related Minerals - Strunz-mindat GroupingHide
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8.BE.05 | Augelite | Al2(PO4)(OH)3 | Mon. 2/m : _B_2/m |
---|---|---|---|
8.BE.10 | Grattarolaite | Fe3+3(PO4)O3 | Trig. 3_m_ : R_3_m |
8.BE.15 | Cornetite | Cu3(PO4)(OH)3 | Orth. m m m _(_2/_m_2/_m_2/m ) : P b c a |
8.BE.20 | Clinoclase | Cu3(AsO4)(OH)3 | Mon. 2/m : _P_21/b |
8.BE.25 | Arhbarite | Cu2Mg(AsO4)(OH)3 | Tric. 1 : _P_1 |
8.BE.25 | Gilmarite | Cu3(AsO4)(OH)3 | Tric. 1 : _P_1 |
8.BE.30 | Allactite | Mn2+7(AsO4)2(OH)8 | Mon. 2/m : _P_21/b |
8.BE.30 | Flinkite | Mn2+2Mn3+(AsO4)(OH)4 | Orth. m m m _(_2/_m_2/_m_2/m ) : P n m a |
8.BE.30 | Raadeite | Mg7(PO4)2(OH)8 | Mon. 2/m |
8.BE.35 | Chlorophoenicite | (Mn,Mg)3Zn2(AsO4)(OH,O)6 | Mon. 2/m : _B_2/m |
8.BE.35 | Magnesiochlorophoenicite | (Mg,Mn)3Zn2(AsO4)(OH,O)6 | Mon. 2/m : _B_2/m |
8.BE.35 | Mineral E (of Dunn, et. al., 1982) | Orth. m m m _(_2/_m_2/_m_2/m ) | |
8.BE.40 | Gerdtremmelite | (Zn,Fe)(Al,Fe)2(AsO4)(OH)5 | Tric. |
8.BE.45 | Dixenite | CuMn2+14Fe2+(SiO4)2(As5+O4)(As3+O3)5(OH)6 | Trig. 3 : _R_3 |
8.BE.45 | Hematolite | (Mn,Mg,Al,Fe3+)15(As5+O4)2(As3+O3)(OH)23 | Trig. 3 : _R_3 |
8.BE.45 | Kraisslite | Zn3(Mn,Mg)25(Fe3+,Al)(As3+O3)2[(Si,As5+)O4]10(OH)16 | Orth. 222 : _C_2221 |
8.BE.45 | Mcgovernite | Mn19Zn3(AsO4)3(AsO3)(SiO4)3(OH)21 | Trig. 3_m_ _(_32/m ) |
8.BE.45 | Arakiite | (Zn,Mn2+)(Mn2+,Mg)12(Fe3+,Al)2(As5+O4)2(As3+O3)(OH)23 | Mon. m : B b |
8.BE.45 | Turtmannite | (Mn,Mg)22.5Mg3-3x((V5+,As5+)O4)3(As3+O3)x(SiO4)3O5-5x(OH)20+x | Trig. |
8.BE.45 | Carlfrancisite | Mn2+3(Mn2+,Mg,Fe3+,Al)42[As3+O3]2(As5+O4)4[(Si,As5+)O4]6[(As5+,Si)O4]2(OH)42 | Trig. 3_m_ _(_32/m ) : R_3_c |
8.BE.50 | Synadelphite | Mn2+9(As5+O4)2(As3+O3)(OH)9 · 2H2O | Orth. m m m _(_2/_m_2/_m_2/m ) : P n m a |
8.BE.55 | Holdenite | (Mn2+,Mg)6Zn3(AsO4)2(SiO4)(OH)8 | Orth. m m m _(_2/_m_2/_m_2/m ) : C c c a |
8.BE.60 | Kolicite | Mn2+7Zn4(AsO4)2(SiO4)2(OH)8 | Orth. m m m _(_2/_m_2/_m_2/m ) : C m c a |
8.BE.65 | Sabelliite | (Cu,Zn)2Zn(AsO4,SbO4)(OH)3 | Trig. 3 : _P_3 |
8.BE.70 | Jarosewichite | Mn2+3Mn3+(AsO4)(OH)6 | Orth. 222 |
8.BE.75 | Theisite | Cu5Zn5(AsO4,SbO4)2(OH)14 | Orth. |
8.BE.80 | Coparsite | Cu4(AsO4,VO4)O2Cl | Orth. m m m _(_2/_m_2/_m_2/m ) : P b c m |
8.BE.85 | Waterhouseite | Mn2+7(PO4)2(OH)8 | Mon. 2/m : _P_21/b |
8.BE.90 | Vasilseverginite | Cu9O4(AsO4)2(SO4)2 | Mon. 2/m |
Fluorescence of ArganditeHide
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Other InformationHide
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Notes:
Slowly soluble in cold 10% 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 ArganditeHide
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References for ArganditeHide
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Reference List:
Brugger, J., Elliott, P., Meisser, N., Ansermet, S. (2011) Argandite, Mn7(VO4)2(OH)8, the V analogue of allactite from the metamorphosed Mn ores at Pipji, Turtmann Valley, Switzerland. American Mineralogist, 96 (11) 1894-1900 doi:10.2138/am.2011.3841
Localities for ArganditeHide
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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.
Italy | |
---|---|
Liguria Genoa Ne Reppia ⓘ Gambatesa Mine | SCXRD: L. Bindi - University of Firenze ... +1 other reference |
Switzerland (TL) | |
Valais Leuk Turtmann-Unterems Turtmann Valley ⓘ Pipjitälli (TL) | Williams et al. (2010) +1 other reference |
ⓘ Pipji glacier | Ansermet (2012) |