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Strontioginorite

A valid IMA mineral species - grandfathered
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About StrontioginoriteHide

Formula:
CaSrB14O20(OH)6 · 5H2O
Colour:
Colourless
Lustre:
Greasy, Silky
Hardness:
2 - 3
Specific Gravity:
2.25
Crystal System:
Monoclinic
Name:
In allusion to its composition, with dominant strontium and its relationship to Ginorite.
The strontium analogue of ginorite.


Unique IdentifiersHide

Mindat ID:
3741
Long-form identifier:
mindat:1:1:3741:5

IMA Classification of StrontioginoriteHide

Classification of StrontioginoriteHide

6.FC.15

6 : BORATES
F : Hexaborates
C : Phyllo-hexaborates
26.6.7.2

26 : HYDRATED BORATES CONTAINING HYDROXYL OR HALOGEN
6 : Hexaborates
9.3.32

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

Physical Properties of StrontioginoriteHide

Greasy, Silky
Transparency:
Transparent
Colour:
Colourless
Streak:
White
Hardness:
2 - 3 on Mohs scale
Cleavage:
Perfect
(010) perfect, (001) very good
Comment:
Easily deformed
Density:
2.25(1) g/cm3 (Measured)    2.265 g/cm3 (Calculated)

Optical Data of StrontioginoriteHide

Type:
Biaxial (+)
RI values:
nα = 1.512 nβ = 1.524 nγ = 1.577
2V:
Measured: 53° , Calculated: 54°
Max. Birefringence:
δ = 0.065
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.

Surface Relief:
Moderate
Dispersion:
strong

Chemistry of StrontioginoriteHide

Mindat Formula:
CaSrB14O20(OH)6 · 5H2O
Element Weights:
Element% weight
O62.690 %
B19.131 %
Sr11.075 %
Ca5.066 %
H2.038 %

Calculated from ideal end-member formula.

Crystallography of StrontioginoriteHide

Crystal System:
Monoclinic
Class (H-M):
2/m - Prismatic
Space Group:
P21/b
Setting:
P21/a
Cell Parameters:
a = 12.817(8) Å, b = 14.448(8) Å, c = 12.783(8) Å
β = 101.42(8)°
Ratio:
a:b:c = 0.887 : 1 : 0.885
Unit Cell V:
2,320.29 ų (Calculated from Unit Cell)
Morphology:
Forms include (110), (010), and (111). Also (001), (100), (250), (131), (141).

Crystal StructureHide

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IDSpeciesReferenceLinkYearLocalityPressure (GPa)Temp (K)
0006023StrontioginoriteGrice J D (2005) Strontioginorite: crystal-structure analysis and hydrogen bonding The Canadian Mineralogist 43 1019-102620050293
0000214StrontioginoriteKonnert J A, Clark J R, Christ C L (1970) Crystal structure of strontioginorite, (Sr,Ca)2B14O20(OH)6.5H2O American Mineralogist 55 1911-193119700293
CIF Raw Data - click here to close

X-Ray Powder DiffractionHide

Powder Diffraction Data:
d-spacingIntensity
7.25 Å(very strong)
2.10 Å(strong)
5.40 Å(medium)
3.92 Å(medium)
3.34 Å(medium)
1.19 Å(medium)
4.75 Å(medium weak)

Geological EnvironmentHide

Paragenetic Mode(s):
Paragenetic ModeEarliest Age (Ga)
Stage 7: Great Oxidation Event<2.4
47a : [Near-surface hydration of prior minerals]
47c : [Carbonates, phosphates, borates, nitrates]

Type Occurrence of StrontioginoriteHide

General Appearance of Type Material:
Crystals up to 3 mm long, 1 mm wide, and 0.5 mm.
Place of Conservation of Type Material:
National Museum of Natural History, Washington, D.C., USA, 114168.
Associated Minerals at Type Locality:

Synonyms of StrontioginoriteHide

Other Language Names for StrontioginoriteHide

Common AssociatesHide

Associations Based on Photo Data:
3 photos of Strontioginorite associated with AnhydriteCaSO4
2 photos of Strontioginorite associated with GypsumCaSO4 · 2H2O

Related Minerals - Strunz-mindat GroupingHide

6.FC.05NobleiteCaB6O9(OH)2 · 3H2OMon. 2/m
6.FC.05TunelliteSrB6O9(OH)2 · 3H2OMon. 2/m : P21/b
6.FC.10StrontioboriteSr[B8O11(OH)4]Mon. 2 : P21
6.FC.15GinoriteCa2B14O20(OH)6 · 5H2OMon. 2/m : P21/b
6.FC.20FabianiteCaB3O5(OH)Mon. 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 StrontioginoriteHide

References for StrontioginoriteHide

Localities for StrontioginoriteHide

Showing 8 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.
Argentina
 
  • Catamarca Province
    • Antofagasta de la Sierra Department
Helvaci +2 other references
Canada
 
  • New Brunswick
    • Kings Co.
      • Cardwell Parish
Grice et al. (2005)
Grice (2002)
      • Studholm Parish
Grice et al. (2005)
Germany (TL)
 
  • Lower Saxony
    • Göttingen District
      • Bovenden
        • Reyershausen
Braitsch (1959)
  • Thuringia
    • Nordhausen District
      • Harztor
        • Niedersachswerfen
Siemroth (2008)
Kazakhstan
 
  • West Kazakhstan Region
    • Terekti District
      • Aksai Valley
Коротченкова et al. (2016)
Pekov et al. (2020)
 
and/or  
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