Berdesinskiite (original) (raw)
A valid IMA mineral species
About BerdesinskiiteHide
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Specific Gravity:
4.536 (Calculated)
Crystal System:
Monoclinic
Name:
For Professor Waldemar Berdesinski (1911-1990), crystallographer, University of Heidelberg, Heidelberg, Germany.
Unique IdentifiersHide
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Long-form identifier:
mindat:1:1:630:1
08c6c056-599a-4ebe-867e-c0c2939fdf3a
Classification of BerdesinskiiteHide
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Type description reference:
4.CB.30
4 : OXIDES (Hydroxides, V[5,6] vanadates, arsenites, antimonites, bismuthites, sulfites, selenites, tellurites, iodates)
C : Metal: Oxygen = 2: 3,3: 5, and similar
B : With medium-sized cations
7.7.2.1
7 : MULTIPLE OXIDES
7 : AB2X5
7.12.15
7 : Oxides and Hydroxides
12 : Oxides of V, Nb and Ta
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.
Please only use the official IMA–CNMNC symbol. Older variants are listed for historical use only.
Symbol | Source | Reference |
---|---|---|
Bds | IMA–CNMNC | Warr, L.N. (2021). IMA–CNMNC approved mineral symbols. Mineralogical Magazine, 85(3), 291-320. doi:10.1180/mgm.2021.43 |
Brd | The Canadian Mineralogist (2019) | The Canadian Mineralogist (2019) The Canadian Mineralogist list of symbols for rock- and ore-forming minerals (December 30, 2019). download |
Physical Properties of BerdesinskiiteHide
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Density:
4.536 g/cm3 (Calculated)
Optical Data of BerdesinskiiteHide
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Reflectivity:
Wavelength | R1 | R2 |
---|---|---|
400 nm | 16.6% | 17.1% |
420 nm | 17.1% | 17.5% |
440 nm | 17.4% | 18.0% |
460 nm | 17.9% | 18.4% |
480 nm | 18.3% | 18.9% |
500 nm | 18.8% | 19.4% |
520 nm | 19.2% | 19.8% |
540 nm | 19.5% | 20.3% |
560 nm | 19.8% | 20.8% |
580 nm | 20.0% | 21.1% |
600 nm | 20.3% | 21.3% |
620 nm | 20.4% | 21.4% |
640 nm | 20.5% | 21.5% |
660 nm | 20.6% | 21.6% |
680 nm | 20.4% | 21.6% |
700 nm | 20.2% | 21.5% |
Graph shows reflectance levels at different wavelengths (in nm). Top of box is 100%. Peak reflectance is 21.6%.
R1 shown in black, R2 shown in red
Colour in reflected light:
Reddish brown
Chemical Properties of BerdesinskiiteHide
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Crystallography of BerdesinskiiteHide
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Crystal System:
Monoclinic
Cell Parameters:
a = 10.11 Å, b = 5.084 Å, c = 7.03 Å
β = 111.46°
Ratio:
a:b:c = 1.989 : 1 : 1.383
Unit Cell V:
336.29 ų (Calculated from Unit Cell)
Comment:
Point Group: 2/m or m.; Space Group: [C2/c or Cc; P21/c; P2/c or P c] (by analogy to synthetic V2TiO5) ·
Crystal StructureHide
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ID | Species | Reference | Link | Year | Locality | Pressure (GPa) | Temp (K) |
---|---|---|---|---|---|---|---|
0007329 | Berdesinskiite | Armbruster T, Galuskin E V, Reznitsky L Z, Sklyarov E V (2009) X-ray structural investigation of the oxyvanite (V3O5) - berdesinskiite (V2TiO5) series: V4+ substituting for octahedrally coordinated Ti4+ European Journal of Mineralogy 21 885-891 | 2009 | Pereval marble quarry, Sludyanka complex, south of Lake Baikal, Russia | 0 | 293 | |
0007330 | Berdesinskiite | Armbruster T, Galuskin E V, Reznitsky L Z, Sklyarov E V (2009) X-ray structural investigation of the oxyvanite (V3O5) - berdesinskiite (V2TiO5) series: V4+ substituting for octahedrally coordinated Ti4+ European Journal of Mineralogy 21 885-891 | 2009 | Pereval marble quarry, Sludyanka complex, south of Lake Baikal, Russia | 0 | 293 | |
0007331 | Berdesinskiite | Armbruster T, Galuskin E V, Reznitsky L Z, Sklyarov E V (2009) X-ray structural investigation of the oxyvanite (V3O5) - berdesinskiite (V2TiO5) series: V4+ substituting for octahedrally coordinated Ti4+ European Journal of Mineralogy 21 885-891 | 2009 | Pereval marble quarry, Sludyanka complex, south of Lake Baikal, Russia | 0 | 293 |
CIF Raw Data - click here to close
X-Ray Powder DiffractionHide
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Powder Diffraction Data:
d-spacing | Intensity |
---|---|
4.721 Å | ( |
4.492 Å | ( |
3.316 Å | ( |
2.895 Å | ( |
2.676 Å | ( |
2.543 Å | ( |
2.447 Å | ( |
Comments:
Recorded on type material; line intensities not given
Geological EnvironmentHide
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Type Occurrence of BerdesinskiiteHide
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General Appearance of Type Material:
As grains, rarely up to 70 µm, and as rims arouns schreyerite.
Place of Conservation of Type Material:
Universities of Bochum, Hamburg and Heidelberg, Germany;
National Museum of Natural History, Washington, D.C., USA (No. 147362).
Geological Setting of Type Material:
In strongly weathered gneiss with quartzite in a gem kornerupine deposit of Precambrian age.
Associated Minerals at Type Locality:
Reference:
Bernhardt, H.-J. , Schmetzer, K. and Medenbach, O. (1983): Berdesinskiite, V2TiO5, a new mineral from Kenya and additional data for schreyerite, V2Ti3O9. Neues Jahrbuch für Mineralogie, Monatshefte, 3, 110-118.
Synonyms of BerdesinskiiteHide
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Other Language Names for BerdesinskiiteHide
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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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4.CB. | Sassite | Ti3+2Ti4+O5 | Orth. m m m _(_2/_m_2/_m_2/m ) : C m c m |
---|---|---|---|
4.CB. | Ferrohögbomite-2N2S | [(Fe2+,Mg,Zn,Al)3(Al,Ti,Fe3+)8O15(OH)]2 | Hex. 6_m_ m : P_63_m c |
4.CB. | Magnesiohögbomite-6N12S | Mg5Al11TiO23(OH) | Trig. 3_m_ _(_32/m ) : R_3_m |
4.CB. | Griffinite | Al2TiO5 | Orth. m m m _(_2/_m_2/_m_2/m ) : C m c m |
4.CB. | Zhenruite | (MoO3)2 · H2O | Mon. 2/m : _P_21/m |
4.CB. | Pengite | (Pb8Sb3+3)Σ11Sb5+9O35 | Trig. 3_m_ _(_32/m ) : R_3_m |
4.CB. | Virgilluethite | MoO3 · H2O | Mon. 2/m : _P_21/b |
4.CB.05 | Brizziite | NaSb5+O3 | Trig. 3 : _R_3 |
4.CB.05 | Corundum | Al2O3 | Trig. 3_m_ _(_32/m ) : R_3_c |
4.CB.05 | Ecandrewsite | (Zn,Fe2+,Mn2+)TiO3 | Trig. 3 : _R_3 |
4.CB.05 | Eskolaite | Cr2O3 | Trig. 3_m_ _(_32/m ) : R_3_c |
4.CB.05 | Geikielite | MgTiO3 | Trig. 3 : _R_3 |
4.CB.05 | Hematite | Fe2O3 | Trig. 3_m_ _(_32/m ) : R_3_c |
4.CB.05 | Ilmenite | Fe2+TiO3 | Trig. 3 : _R_3 |
4.CB.05 | Karelianite | V3+2O3 | Trig. 3_m_ _(_32/m ) : R_3_c |
4.CB.05 | Melanostibite | Mn2+2Fe3+Sb5+O6 | Trig. 3 : _R_3 |
4.CB.05 | Pyrophanite | Mn2+TiO3 | Trig. 3 : _R_3 |
4.CB.05 | Akimotoite | (Mg,Fe2+)SiO3 | Trig. 3 : _R_3 |
4.CB.05 | Auroantimonate | AuSbO3 | |
4.CB.05 | UM1998-11-O-AuHSb | Au+2Sb3+O2(OH) | |
4.CB.05 | Tistarite | Ti3+2O3 | Trig. 3_m_ _(_32/m ) : R_3_c |
4.CB.05 | Unnamed (Fe-Cr Oxide) | FeCrO3 | Trig. 3 : _R_3 |
4.CB.05 | Hemleyite | (Fe2+0.48Mg0.37Ca0.04Na0.04Mn2+0.03Al0.03Cr3+0.01)sum=1.00Si1.00O3 | Trig. 3 : _R_3 |
4.CB.10 | Avicennite | Tl2O3 | Iso. m_3(2/m_3) : I _a_3 |
4.CB.10 | Bixbyite-(Mn) | Mn3+2O3 | Iso. m_3(2/m_3) : I _a_3 |
4.CB.10 | Bixbyite-(Fe) | (Fe,Mn)2O3 | Iso. |
4.CB.15 | Armalcolite | (Mg,Fe2+)Ti2O5 | Orth. m m m _(_2/_m_2/_m_2/m ) |
4.CB.15 | Pseudobrookite | Fe2TiO5 | Orth. m m m _(_2/_m_2/_m_2/m ) |
4.CB.15 | Ferropseudobrookite | Fe2+Ti2O5 | Orth. m m m _(_2/_m_2/_m_2/m ) : C m c m |
4.CB.20 | Zincohögbomite-2N2S | [(Zn,Al,Fe2+)3(Al,Fe3+,Ti)8O15(OH)]2 | Hex. 6_m_ m : P_63_m c |
4.CB.20 | Zincohögbomite-2N6S | [(Zn,Mg)7(Al,Fe3+,Ti)16O31(OH)]2 | Hex. 6_m_ m : P_63_m c |
4.CB.20 | Magnesiohögbomite-6N6S | [(Mg,Fe2+)3(Al,Ti,Fe3+)8O15(OH)]6 | Trig. 3_m_ _(_32/m ) : R_3_m |
4.CB.20 | Magnesiohögbomite-2N3S | [(Mg,Fe2+,Zn)4(Al,Ti,Fe3+)10O19(OH)]2 | Trig. 3_m_ _(_32/m ) : P_31_m |
4.CB.20 | Magnesiohögbomite-2N2S | [(Mg,Fe2+)3[Al7(Ti,Fe3+)]O15(OH)]2 | Hex. 6_m_ m : P_63_m c |
4.CB.20 | Ferrohögbomite-6N12S | [(Fe2+,Mg,Zn)5(Al,Ti,Fe3+)12O23(OH)]6 | Trig. 3_m_ _(_32/m ) : R_3_m |
4.CB.20 | Magnesiohögbomite-2N4S | (Mg8.43Fe2+1.57)sum=10Al22Ti4+2O46(OH)2 | Hex. 6_m_ m : P_63_m c |
4.CB.20 | Magnesiobeltrandoite-2N3S | (Mg6Al2)(Al18Fe3+2)O38(OH)2 | Trig. 3_m_ : _P_3_m_1 |
4.CB.20 | Zincovelesite-6N6S | Zn3(Fe3+,Mn3+,Al,Ti)8O15(OH) | Trig. 3_m_ _(_32/m ) : _P_3_m_1 |
4.CB.25 | Pseudorutile | Fe2Ti3O9 | Hex. 622 : _P_6322 |
4.CB.25 | Kleberite | FeTi6O11(OH)5 | Mon. 2/m : _P_21/b |
4.CB.30 | Oxyvanite | V3+2V4+O5 | Mon. 2/m : _B_2/b |
4.CB.30 | Kaitianite | Ti3+2Ti4+O5 | Mon. 2/m : _B_2/b |
4.CB.35 | Olkhonskite | (Cr,V)2Ti3O9 | Mon. |
4.CB.35 | Schreyerite | V3+2Ti3O9 | Mon. 2/m : _B_2/b |
4.CB.35 | Machiite | Al2Ti3O9 | Mon. 2/m : _B_2/b |
4.CB.35 | Vestaite | (Ti4+Fe2+)Ti4+3O9 | Mon. 2/m : _B_2/b |
4.CB.40 | Kamiokite | Fe2Mo3O8 | Hex. 6_m_ m : P_63_m c |
4.CB.40 | Nolanite | V3+8Fe3+2O14(OH)2 | Hex. 6_m_ m : P_63_m c |
4.CB.40 | Rinmanite | Zn2Sb2Mg2Fe4O14(OH)2 | Hex. 6 : _P_63 |
4.CB.40 | Iseite | Mn2Mo3O8 | Hex. 6_m_ m : P_63_m c |
4.CB.40 | Majindeite | Mg2Mo3O8 | Hex. 6_m_ m : P_63_m c |
4.CB.45 | Claudetite | As2O3 | Mon. 2/m |
4.CB.45 | Stibioclaudetite | AsSbO3 | Mon. 2/m : _P_21/m |
4.CB.50 | Arsenolite | As2O3 | Iso. m_3_m _(_4/_m_32/m ) : F d_3_m |
4.CB.50 | Senarmontite | Sb2O3 | Iso. m_3_m _(_4/_m_32/m ) : F d_3_m |
4.CB.55 | Valentinite | Sb2O3 | Orth. m m m _(_2/_m_2/_m_2/m ) : P c c n |
4.CB.60 | Bismite | Bi2O3 | Mon. 2/m : _P_21/b |
4.CB.65 | Sphaerobismoite | Bi2O3 | Tet. |
4.CB.70 | Sillénite | Bi12SiO20 | Iso. 23 : _I_23 |
4.CB.75 | Kyzylkumite | V3+Ti2O5(OH) | Mon. 2/m : _P_21/b |
4.CB.80 | Tietaiyangite | Fe3+4Fe2+TiO9 | Hex. |
4.CB.85 | Liuite | FeTiO3 | Orth. m m m _(_2/_m_2/_m_2/m ) : P n m a |
4.CB.90 | Luogufengite | Fe2O3 | Orth. m _m_2 : P n _a_21 |
4.CB.95 | Wangdaodeite | FeTiO3 | Trig. 3_m_ : R_3_c |
Other InformationHide
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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 BerdesinskiiteHide
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References for BerdesinskiiteHide
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Reference List:
Localities for BerdesinskiiteHide
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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.