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Byrudite

A valid IMA mineral species
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About ByruditeHide

Formula:
(Be,◻)(V3+,Ti,Cr)3O6
ideal formula (by analogy to norbergite): V23+Ti(BeO4)O2
Colour:
Black
Lustre:
Metallic
Hardness:
7
Specific Gravity:
4.35
Crystal System:
Orthorhombic
Name:
Named by G. Raade, T. Balić-Žunić, and C.J. Stanley after the type locality of Byrud Emerald Mine, Norway.
Isostructural with:
A mineral related to kyzylkumite. It is the V analogue of (the recently approved) verbierite. Unique combination of elements; also the only currently (2025) known Be-V mineral.

Byrudite has a norbergite-type structure. It consists of kinked chains of edge-sharing V and Ti octahedra. These polyhedra are interconnected by isolated BeO4 tetrahedra. It is suggested that F and OH are not present, which would be consistent with the substitution of "sellaite" component of norbergite by "rutile" component.


Unique IdentifiersHide

Mindat ID:
43917
Long-form identifier:
mindat:1:1:43917:4

Similar NamesHide

BairditeA valid IMA mineral speciesPb2Cu42+Te26+O10(OH)2(SO4) · H2O
BarititeA synonym of Baryte
BorditeA synonym of Okenite
BuratiteA synonym of Aurichalcite
BurtiteA valid IMA mineral speciesCa[Sn(OH)6]

IMA Classification of ByruditeHide

Approved
IMA Formula:
(Be,◻)(V3+,Ti4+)3O6
Approval year:
2013

Classification of ByruditeHide

4.CA.

4 : OXIDES (Hydroxides, V[5,6] vanadates, arsenites, antimonites, bismuthites, sulfites, selenites, tellurites, iodates)
C : Metal: Oxygen = 2: 3,3: 5, and similar
A : With small cations

Mineral SymbolsHide

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

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

Physical Properties of ByruditeHide

Metallic
Transparency:
Opaque
Colour:
Black
Streak:
Black
Hardness:
Hardness:
VHN100=1493 - Vickers
Comment:
~7, based on indentation measurements
Tenacity:
Brittle
Cleavage:
None Observed
Fracture:
Irregular/Uneven
Density:
4.35 g/cm3 (Measured)    
Comment:
Calculated for the empirical formula with 0.84 Be apfu

Optical Data of ByruditeHide

Anisotropism:
Weak
Bireflectance:
Weak
Reflectivity:
WavelengthR1 (%)R2 (%)
470nm16.6%17.5%
546nm16.7%17.9%
589nm16.8%18.3%
650nm16.8%18.6%


Graph shows reflectance levels at different wavelengths (in nm). Peak reflectance is 18.6%.
R1 shown in black, R2 shown in red
Colour in reflected light:
Gray
Internal Reflections:
not present
Pleochroism:
Non-pleochroic

Chemistry of ByruditeHide

Mindat Formula:
(Be,◻)(V3+,Ti,Cr)3O6

ideal formula (by analogy to norbergite): V23+Ti(BeO4)O2
Element Weights:
Element% weight
V59.273 %
O37.232 %
Be3.495 %

Calculated from ideal end-member formula.
V
O
Be
Common Impurities:
Ti,Cr,Fe,Al

Crystallography of ByruditeHide

Crystal System:
Orthorhombic
Class (H-M):
mmm(2/m2/m2/m) - Dipyramidal
Space Group:
Pnma
Setting:
Pnma
Cell Parameters:
a = 9.982(1) Å, b = 8.502(1) Å, c = 4.5480(6) Å
Ratio:
a:b:c = 1.174 : 1 : 0.535
Unit Cell V:
385.97 ų
Z:
4
Twinning:
Occurs on {210}.

Crystal StructureHide

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IDSpeciesReferenceLinkYearLocalityPressure (GPa)Temp (K)
0006110ByruditeRaade G, Balic-Zunic T (2006) The crystal structure of (Be,_)(V,Ti)3O6, a mineral related to kyzylkumite The Canadian Mineralogist 44 1147-11582006Byrud farm, Eidsvoll, Akershus, South Norway0293
CIF Raw Data - click here to close

X-Ray Powder DiffractionHide

Powder Diffraction Data:
d-spacingIntensity
4.15 Å(w)
3.72 Å(m)
2.96 Å(s)
2.57 Å(w)
2.48 Å(vw)
2.17 Å(w)
1.68 Å(s)
1.43 Å(w)
Comments:
From Type Description.

Geological EnvironmentHide

Paragenetic Mode(s):
Paragenetic ModeEarliest Age (Ga)
Stage 4b: Highly evolved igneous rocks>3.0
34 : Complex granite pegmatites

Type Occurrence of ByruditeHide

General Appearance of Type Material:
single/intergrown prisms, up to ca. 1 x 0.1 mm, needle- or lath-like; may be striated along the length as a result of twinning on
{210}; six-sided cross sections observed; crystal faces uneven and indistinct
Place of Conservation of Type Material:
Type material is deposited in the collections of the Natural History Museum, University of Oslo, Norway, catalogue number 43570
Geological Setting of Type Material:
Emerald-bearing syenitic pegmatites of Permian age (Byrud); rare, primary magmatic phase within quartz
Associated Minerals at Type Locality:

Synonyms of ByruditeHide

Other Language Names for ByruditeHide

Dutch:Byrudiet
German:Byrudit

Common AssociatesHide

Associations Based on Photo Data:
2 photos of Byrudite associated with FluoriteCaF2
2 photos of Byrudite associated with BerylBe3Al2(Si6O18)
1 photo of Byrudite associated with CoulsoniteFe2+V3+2O4
1 photo of Byrudite associated with SenaitePb(Mn,Y,U)(Fe,Zn)2(Ti,Fe,Cr,V)18(O,OH)38

Related Minerals - Strunz-mindat GroupingHide

4.CA.05VerbieriteBeCr3+2TiO6Orth. mmm(2/m2/m2/m) : Pnma

Fluorescence of ByruditeHide

non-fluorescent

Other InformationHide

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 ByruditeHide

References for ByruditeHide

Localities for ByruditeHide

Showing 3 localities.

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.
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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.
Norway (TL)
 
  • Akershus
    • Eidsvoll
      • Minnesund
Williams et al. (2013) +2 other references
Russia
 
  • Murmansk Oblast
    • Pechengsky District
      • Pechenga Ni-Cu ore field
Minerals 2018 (11) +2 other references
Spain
 
  • Canary Islands
    • Santa Cruz de Tenerife Province
      • Tenerife
Dill et al. (2023)
 
and/or  
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