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Strontioborite

A valid IMA mineral species
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Formula:
Sr[B8O11(OH)4]
Colour:
Colourless
Crystal System:
Monoclinic
Name:
The name reflects its composition : a strontium borate.
Hide all sections | Show all sections

Unique IdentifiersHide

Mindat ID:
3807
Long-form identifier:
mindat:1:1:3807:8
GUID
(UUID V4):
cdcf5ebf-51e0-4846-a593-96ac066fdbc1

IMA Classification of StrontioboriteHide

Approved, Pending publication
Approval history:
first discredited; then (2020) re-approved

Classification of StrontioboriteHide

6.FC.10

6 : BORATES
F : Hexaborates
C : Phyllo-hexaborates
25.6.3.1

25 : ANHYDROUS BORATES CONTAINING HYDROXYL OR HALOGEN
6 : Hexaborates
9.3.26

9 : Borates
3 : Borates of Ca and Sr

Mineral SymbolsHide

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

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

Pronunciation of StrontioboriteHide

Pronunciation:
PlayRecorded byCountry
Jolyon RalphUnited Kingdom

Physical Properties of StrontioboriteHide

Transparency:
Transparent
Colour:
Colourless
Tenacity:
Very brittle

Optical Data of StrontioboriteHide

Type:
Biaxial (+/-)
RI values:
nα = 1.470 nβ = 1.510 nγ = 1.579
2V:
Measured: 85° , Calculated: 78°
Max Birefringence:
δ = 0.109
Image shows birefringence interference colour range (at 30µm thickness)
and does not take into account mineral colouration.
Surface Relief:
Low
Dispersion:
relatively weak

Chemistry of StrontioboriteHide

Mindat Formula:
Sr[B8O11(OH)4]

Crystallography of StrontioboriteHide

Crystal System:
Monoclinic
Class (H-M):
2 - Sphenoidal
Space Group:
P21
Setting:
P21
Cell Parameters:
a = 7.6192(3) Å, b = 8.1867(2) Å, c = 9.9164(3) Å
β = 108.357(4)°
Ratio:
a:b:c = 0.931 : 1 : 1.211
Unit Cell V:
587.07 ų (Calculated from Unit Cell)

X-Ray Powder DiffractionHide

Powder Diffraction Data:
d-spacingIntensity
7.22 Å(100)
5.409 Å(61)
4.090 Å(64)
3.300 Å(48)
3.082 Å(28)
2.926 Å(25)
2.121 Å(30)
2.043 Å(37)

Type Occurrence of StrontioboriteHide

Place of Conservation of Type Material:
collections of the Fersman Mineralogical Museum, Russian Academy of Sciences, Leninskiy Prospekt 18-2, Moscow 119071, Russia, registration numbers 69851 (holotype) and ST-7069 (cotype)

Synonyms of StrontioboriteHide

Other Language Names for StrontioboriteHide

Related Minerals - Strunz-mindat GroupingHide

6.FC.05TunelliteSrB6O9(OH)2 · 3H2OMon. 2/m : P21/b
6.FC.05NobleiteCaB6O9(OH)2 · 3H2OMon. 2/m
6.FC.15GinoriteCa2B14O20(OH)6 · 5H2OMon. 2/m : P21/b
6.FC.15StrontioginoriteCaSrB14O20(OH)6 · 5H2OMon. 2/m : P21/b
6.FC.20FabianiteCaB3O5OHMon. 2/m : P21/b

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 StrontioboriteHide

References for StrontioboriteHide

Localities for StrontioboriteHide

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

- 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.
Kazakhstan (TL)
 
  • Aktobe Region
    • Shalkar District
      • Aksai Valley
Handbook of Mineralogy Vol V p 6 +2 other references
 
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