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Shimazakiite

A valid IMA mineral species
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About ShimazakiiteHide

08620400017272472068901.jpg
Dr. Hidehiko Shimazaki
Formula:
Ca2B2-xO5-3x(OH)3x (x = 0~0.06)
3 OH partially replace 1 BO3 group.
Colour:
Grayish white
Lustre:
Vitreous
Crystal System:
Monoclinic
Name:
Named in honor of Dr. Hidehiko Shimazaki (島崎英彦) (2 June 1939, Tokyo, Japan), professor emeritus of Tokyo University, in recognition of his contributions to skarn mineralogy.
Compare also the closely related Datolite and its B-rich variety Bakerite.

Two polytypes (4M and 4O) are known.


Unique IdentifiersHide

Mindat ID:
41969
Long-form identifier:
mindat:1:1:41969:3

IMA Classification of ShimazakiiteHide

Classification of ShimazakiiteHide

6.BC.25

6 : BORATES
B : Diborates
C : Ino-diborates with triangles and/or tetrahedra

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

Physical Properties of ShimazakiiteHide

Vitreous
Colour:
Grayish white
Streak:
White
Tenacity:
Brittle
Cleavage:
None Observed
Fracture:
Irregular/Uneven

Optical Data of ShimazakiiteHide

Type:
Biaxial (-)
Pleochroism:
Non-pleochroic

Chemistry of ShimazakiiteHide

Mindat Formula:
Ca2B2-xO5-3x(OH)3x (x = 0~0.06)

3 OH partially replace 1 BO3 group.

Crystallography of ShimazakiiteHide

Polytype:
Formula:
Crystal System:
Class (H-M)
Space Group:
Space Group Setting:
Cell Parameters:
Ratio:
Unit Cell Volume (calc):
Z:
Comment:
Shimazakiite-4MShimazakiite-4O
Ca2B2-xO5-3x(OH)3x (x = 0~0.06)Ca2B2-xO5-3x(OH)3x (x = 0~0.06)
Monoclinic Orthorhombic 
2/m - Prismatic222 - Disphenoidal
P21/cP212121
P21/c 
a = 3.5485(12) Å, b = 6.352(2) Å, c = 19.254(6) Å
β = 92.393(13)°
a = 3.55645(18) Å, b = 6.35194(15) Å, c = 19.2534(5) Å
a:b:c = 0.559 : 1 : 3.031a:b:c = 0.56 : 1 : 3.031
V 433.61 ų
(Calculated from Unit Cell)
V 434.94 ų
(Calculated from Unit Cell)
44
  

X-Ray Powder DiffractionHide

Geological EnvironmentHide

Paragenetic Mode(s):
Paragenetic ModeEarliest Age (Ga)
Near-surface Processes
23 : Subaerial aqueous alteration by non-redox-sensitive fluids (see also #47)

Type Occurrence of ShimazakiiteHide

General Appearance of Type Material:
Shimazakiite forms aggregates up to 3 mm where shimazakiite-4M tends to occur in nanometer-sized twin lamellae and shimazakiite-4O in micrometer-sized lamellae.
Place of Conservation of Type Material:
National Museum of Nature and Science, Tokyo, Japan.
Geological Setting of Type Material:
In irregular vein in crystalline limestone near gehlenite-spurrite skarns
Associated Minerals at Type Locality:

Synonyms of ShimazakiiteHide

Other Language Names for ShimazakiiteHide

Japanese:島崎石

Common AssociatesHide

Associations Based on Photo Data:
3 photos of Shimazakiite associated with HenmiliteCa2Cu[B(OH)4]2(OH)4

Related Minerals - Strunz-mindat GroupingHide

6.BC.10CalciboriteCa(B2O4)Orth. mmm(2/m2/m2/m) : Pccn
6.BC.15VimsiteCaB2O2(OH)4Mon. 2/m : B2/b
6.BC.20ParasibirskiteCa2(B2O5) · H2OMon. 2/m : P21/m
6.BC.20SibirskiteCa2(HB2O5)(OH)Mon. 2/m : P21/c

Fluorescence of ShimazakiiteHide

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 ShimazakiiteHide

References for ShimazakiiteHide

Localities for ShimazakiiteHide

Showing 1 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.
Japan (TL)
 
  • Okayama Prefecture
    • Takahashi City
      • Bitchū
        • Fuka
Williams et al. (2011) +3 other references
 
and/or  
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