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Bromellite

A valid IMA mineral species - grandfathered
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About BromelliteHide

04272280017271921851055.jpg
Magnus Bromelius
Formula:
BeO
Colour:
White to creamy white
Lustre:
Vitreous
Hardness:
9
Specific Gravity:
3.017
Crystal System:
Hexagonal
Name:
For Magnus von Bromell (1679-1731), Swedish physician and mineralogist.
A beryllium oxide mineral found in desilicated, skarn-like deposit and as a result of hydrothermal alteration of nepheline in nepheline syenites pegmatites.


Unique IdentifiersHide

Mindat ID:
784
Long-form identifier:
mindat:1:1:784:1

Similar NamesHide

BoromulliteA valid IMA mineral speciesAl9BSi2O19
BrammalliteA variety of ParagoniteNaAl2(AlSi3O10)(OH)2
BromliteA synonym of Alstonite

IMA Classification of BromelliteHide

Classification of BromelliteHide

4.AB.20

4 : OXIDES (Hydroxides, V[5,6] vanadates, arsenites, antimonites, bismuthites, sulfites, selenites, tellurites, iodates)
A : Metal: Oxygen = 2:1 and 1:1
B : M:O = 1:1 (and up to 1:1.25); with small to medium-sized cations only
4.2.2.2

4 : SIMPLE OXIDES
2 : AX
7.4.1

7 : Oxides and Hydroxides
4 : Oxides of Be, Mg and the alkaline earths

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

Physical Properties of BromelliteHide

Vitreous
Transparency:
Transparent
Colour:
White to creamy white
Hardness:
Cleavage:
Distinct/Good
on {1010}
Density:
3.017 g/cm3 (Measured)    3.044 g/cm3 (Calculated)

Optical Data of BromelliteHide

Type:
Uniaxial (+)
RI values:
nω = 1.705 - 1.719 nε = 1.733
Max. Birefringence:
δ = 0.014 - 0.028
Based on recorded range of RI values above.

Interference Colours:
The colours simulate birefringence patterns seen in thin section under crossed polars. They do not take into account mineral colouration or opacity.

Michel-Levy Bar The default colours simulate the birefringence range for a 30 µm thin-section thickness. Adjust the slider to simulate a different thickness.

Grain Simulation You can rotate the grain simulation to show how this range might look as you rotated a sample under crossed polars. Each grain retains its interference colour (retardation) while its brightness falls to black at extinction and reaches a maximum between extinction positions.

Surface Relief:
Very High (positive)
Relative to Canada balsam mounting medium (n ≈ 1.537).

This shows the grain boundary and Becke line effect under plane-polarised light, based on the contrast between this mineral's average refractive index and the mounting medium. It does not take into account mineral colouration.
In focus
Interference Figure:
This shows the idealized uniaxial interference figure - the conoscopic (convergent-light, Bertrand-lens-in) view, for a grain cut with the optic axis centred and vertical. The coloured rings are isochromatics, computed with the same physics as the Michel-Lévy bar above; the dark cross is the isogyre.

For a genuinely uniaxial mineral viewed this way, that cross stays perfectly stationary if you rotate the stage - unlike a biaxial mineral, where it splits apart on rotation. That invariance is itself the standard diagnostic test for telling uniaxial and biaxial minerals apart at the microscope.

Chemistry of BromelliteHide

Mindat Formula:
BeO
Element Weights:
Element% weight
O63.968 %
Be36.032 %

Calculated from ideal end-member formula.
Common Impurities:
Al,B,Ba,Ca,Fe,Mg,Si

Chemical AnalysisHide

Crystallography of BromelliteHide

Crystal System:
Hexagonal
Class (H-M):
6mm - Dihexagonal Pyramidal
Space Group:
P63mc
Cell Parameters:
a = 2.6983(4) Å, c = 4.3776(4) Å
Ratio:
a:c = 1 : 1.622
Unit Cell V:
27.60 ų (Calculated from Unit Cell)
Z:
2
Morphology:
As prismatic crystals, elongated along [0001], to 1 mm, showing pyramidal hemimorphism, with {0001} and {1010} well developed, {1011} small, may be tabular parallel to {0001}; in randomly intergrown rosettelike aggregates; also as cleavage fragments, to 10 cm.
Comment:
synthetic

Crystal StructureHide

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IDSpeciesReferenceLinkYearLocalityPressure (GPa)Temp (K)
0019185BromelliteHazen R M, Finger L W (1986) High-pressure and high-temperature crystal chemistry of beryllium oxide Journal of Applied Physics 59 3728-37331986Synthetic0293
0019179BromelliteHazen R M, Finger L W (1986) High-pressure and high-temperature crystal chemistry of beryllium oxide Journal of Applied Physics 59 3728-37331986Synthetic0293
0019178BromelliteHazen R M, Finger L W (1986) High-pressure and high-temperature crystal chemistry of beryllium oxide Journal of Applied Physics 59 3728-37331986Synthetic0293
0019177BromelliteHazen R M, Finger L W (1986) High-pressure and high-temperature crystal chemistry of beryllium oxide Journal of Applied Physics 59 3728-37331986Synthetic0293
0019176BromelliteHazen R M, Finger L W (1986) High-pressure and high-temperature crystal chemistry of beryllium oxide Journal of Applied Physics 59 3728-37331986Synthetic0293
0019186BromelliteHazen R M, Finger L W (1986) High-pressure and high-temperature crystal chemistry of beryllium oxide Journal of Applied Physics 59 3728-37331986Synthetic0543
0019187BromelliteHazen R M, Finger L W (1986) High-pressure and high-temperature crystal chemistry of beryllium oxide Journal of Applied Physics 59 3728-37331986Synthetic0763
0019188BromelliteHazen R M, Finger L W (1986) High-pressure and high-temperature crystal chemistry of beryllium oxide Journal of Applied Physics 59 3728-37331986Synthetic0963
0019189BromelliteHazen R M, Finger L W (1986) High-pressure and high-temperature crystal chemistry of beryllium oxide Journal of Applied Physics 59 3728-37331986Synthetic01073
0019190BromelliteHazen R M, Finger L W (1986) High-pressure and high-temperature crystal chemistry of beryllium oxide Journal of Applied Physics 59 3728-37331986Synthetic01183
0019180BromelliteHazen R M, Finger L W (1986) High-pressure and high-temperature crystal chemistry of beryllium oxide Journal of Applied Physics 59 3728-37331986Synthetic1.1293
0019181BromelliteHazen R M, Finger L W (1986) High-pressure and high-temperature crystal chemistry of beryllium oxide Journal of Applied Physics 59 3728-37331986Synthetic2.2293
0019182BromelliteHazen R M, Finger L W (1986) High-pressure and high-temperature crystal chemistry of beryllium oxide Journal of Applied Physics 59 3728-37331986Synthetic3.8293
0019183BromelliteHazen R M, Finger L W (1986) High-pressure and high-temperature crystal chemistry of beryllium oxide Journal of Applied Physics 59 3728-37331986Synthetic4293
0019184BromelliteHazen R M, Finger L W (1986) High-pressure and high-temperature crystal chemistry of beryllium oxide Journal of Applied Physics 59 3728-37331986Synthetic5293
0015173BromelliteXu Y N, Ching W Y (1993) Electronic, optical, and structural properties of some wurtzite crystals Physical Review B48 4335-435119930293
0011539BromelliteWyckoff R W G (1963) Second edition. Interscience Publishers, New York, New York Crystal Structures 1 85-23719630293
0017437BromelliteZachariasen W (1925) Ueber die Kristallstruktur von BeO _cod_database_code 1010526 Norsk Geologisk Tidsskrift 8 189-20019250293
0017664BromelliteAminoff G (1925) Ueber Berylliumoxyd als Mineral und dessen Kristallstruktur. _cod_database_code 1010943 Zeitschrift fur Kristallographie 62 113-12219250293
CIF Raw Data - click here to close

X-Ray Powder DiffractionHide

Powder Diffraction Data:
d-spacingIntensity
2.061 Å(100)
2.337 Å(91)
2.189 Å(61)
1.349 Å(29)
1.238 Å(24)
1.598 Å(22)
1.1482 Å(16)
Comments:
Recorded on synthetic material

Geological EnvironmentHide

Paragenetic Mode(s):
Paragenetic ModeEarliest Age (Ga)
Near-surface Processes
23 : Subaerial aqueous alteration by non-redox-sensitive fluids (see also #47)
Stage 4b: Highly evolved igneous rocks>3.0
35 : Ultra-alkali and agpaitic igneous rocks
Stage 7: Great Oxidation Event<2.4
47h : [Near-surface oxidized, dehydrated minerals]

Type Occurrence of BromelliteHide

General Appearance of Type Material:
White hexagonal crystals
Place of Conservation of Type Material:
Swedish Museum of Natural History, Stockholm, Sweden
Geological Setting of Type Material:
In hydrothermal calcite veins and veinlets in hematite skarn and skarnized limestones
Associated Minerals at Type Locality:

Other Language Names for BromelliteHide

German:Bromellit
Simplified Chinese:铍石
Spanish:Bromellita
Traditional Chinese:鈹石

Common AssociatesHide

Associations Based on Photo Data:
4 photos of Bromellite associated with HelvineBe3Mn2+4(SiO4)3S
4 photos of Bromellite associated with ChrysoberylBeAl2O4
4 photos of Bromellite associated with PhlogopiteKMg3(AlSi3O10)(OH)2
3 photos of Bromellite associated with LiberiteLi2BeSiO4
3 photos of Bromellite associated with PhenakiteBe2SiO4
2 photos of Bromellite associated with AmesiteMg2Al(AlSiO5)(OH)4
2 photos of Bromellite associated with FluoriteCaF2
2 photos of Bromellite associated with MagnesioferriteMgFe3+2O4
2 photos of Bromellite associated with DiasporeAlO(OH)
1 photo of Bromellite associated with RhodoniteCaMn3Mn[Si5O15]

Related Minerals - Strunz-mindat GroupingHide

4.AB.'Carbon Monoxide Ice'CO
4.AB.05CredneriteCu+Mn3+O2Mon. 2/m : B2/m
4.AB.10TenoriteCuOMon. 2/m : B2/b
4.AB.15McconnelliteCuCrO2Trig. 3m : R3m
4.AB.15DelafossiteCu+Fe3+O2Trig. 3m(32/m) : R3m
4.AB.20ZinciteZnOHex. 6mm : P63mc
4.AB.25BunseniteNiOIso. m3m(4/m32/m) : Fm3m
4.AB.25PericlaseMgOIso. m3m(4/m32/m) : Fm3m
4.AB.25LimeCaOIso. m3m(4/m32/m) : Fm3m
4.AB.25ManganositeMnOIso. m3m(4/m32/m) : Fm3m
4.AB.25MonteponiteCdOIso. m3m(4/m32/m) : Fm3m
4.AB.25WüstiteFeOIso. m3m(4/m32/m) : Fm3m
4.AB.30PalladinitePdOTet. 4/mmm(4/m2/m2/m) : P42/mmc
4.AB.35'Hongquiite'TiO

Fluorescence of BromelliteHide

Yellowish white in both LW and SW UV

Other InformationHide

Electrical:
Pyroelectric
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 BromelliteHide

References for BromelliteHide

Reference List:

Localities for BromelliteHide

Showing 12 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.
Australia
 
  • New South Wales
    • Clive Co.
Henley et al. (2001)
China
 
  • Hunan
    • Chenzhou
      • Linwu Co.
        • Xianghualing Sn-polymetallic ore field
Xihuan Zhang and Yufeng Ren (2008)
France
 
  • Occitanie
    • Pyrénées-Orientales
      • Céret
        • Prats-de-Mollo-la-Preste
Dubru. M (1986)
Norway
 
  • Telemark
    • Porsgrunn
      • Auenlandet
        • Sagåsen
Larsen et al. (1987) +1 other reference
Russia
 
  • Murmansk Oblast
[World of Stones 95:5-6
  • Republic of Karelia
    • Pitkyarantsky District
Ivashchenko et al. (2006)
  • Sverdlovsk Oblast
    • Malyshevo
      • Malyshevskoe deposit
Avdonin V.N. (2004)
Sweden (TL)
 
  • Värmland County
    • Filipstad
      • Långban Ore District
Aminoff (1925) +2 other references
Jonsson (2003)
Lorin (2003)
      • Persberg ore district
        • Pajsberg
Österberg et al. (2003)
 
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