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Ohmilite

A valid IMA mineral species
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About OhmiliteHide

Formula:
Sr3(Ti,Fe3+)(Si4O12)(O,OH) · 2-3H2O
Colour:
Pink to pinkish brown
Hardness:
Specific Gravity:
3.38
Crystal System:
Monoclinic
Name:
Named in 1973 by Masayuki Komatsu, Kazuya Chihara, and Tadato Mizota after the type locality of Ohmi, Niigata Prefecture, Central Japan.
The Ti- (or rather Ti-O)-analogue of yuzuxiangite.


Unique IdentifiersHide

Mindat ID:
2963
Long-form identifier:
mindat:1:1:2963:2
GUID
(UUID V4):
6d4fdf3c-4f7f-43af-b372-545d50286c47

IMA Classification of OhmiliteHide

Classification of OhmiliteHide

9.DH.10

9 : SILICATES (Germanates)
D : Inosilicates
H : Inosilicates with 4-periodic single chains, Si4O12
65.3.4.3

65 : INOSILICATES Single-Width,Unbranched Chains,(W=1)
3 : Single-Width Unbranched Chains, W=1 with chains P=4
14.9.7

14 : Silicates not Containing Aluminum
9 : Silicates of Ti

Mineral SymbolsHide

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

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

Physical Properties of OhmiliteHide

Transparency:
Translucent
Colour:
Pink to pinkish brown
Streak:
White
Hardness:
3½ on Mohs scale
Cleavage:
Perfect
Parallel to (100)
Density:
3.38 g/cm3 (Measured)    3.394 g/cm3 (Calculated)

Optical Data of OhmiliteHide

Type:
Biaxial
RI values:
nα = 1.649 nγ = 1.715
Max Birefringence:
δ = 0.066
Image shows birefringence interference colour range (at 30µm thickness)
and does not take into account mineral colouration.
Surface Relief:
Moderate
Dispersion:
r < v strong
Pleochroism:
Weak
Comments:
Very weak, colourless to light pink.

Chemistry of OhmiliteHide

Mindat Formula:
Sr3(Ti,Fe3+)(Si4O12)(O,OH) · 2-3H2O

Crystallography of OhmiliteHide

Crystal System:
Monoclinic
Class (H-M):
2/m - Prismatic
Space Group:
P21/m
Setting:
P21/m
Cell Parameters:
a = 10.97 Å, b = 7.79 Å, c = 7.81 Å
β = 100.9°
Ratio:
a:b:c = 1.408 : 1 : 1.003
Unit Cell V:
655.37 ų (Calculated from Unit Cell)
Z:
2

Crystal StructureHide

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IDSpeciesReferenceLinkYearLocalityPressure (GPa)Temp (K)
0000908OhmiliteMizota T, Komatsu M, Chihara K (1983) A refinement of the crystal structure of ohmilite, Sr3(Ti,Fe3+)(O,OH)(Si2O6)2* 2-3H2O American Mineralogist 68 811-81719830293
0014415OhmiliteMizota T, Komatsu M, Chihara K (1973) On the crystal structure of Sr3TiSi4O12(OH)*2H2O, a new mineral Mineralogical Journal 7 302-3051973Ohmi District, Niigata Prefecture, Central Japan0293
CIF Raw Data - click here to close

X-Ray Powder DiffractionHide

Powder Diffraction Data:
d-spacingIntensity
10.83 Å(70)
5.39 Å(77)
4.62 Å(100)
3.83 Å(90)
3.471 Å(42)
3.409 Å(40)
3.264 Å(85)
3.037 Å(80)
2.831 Å(54)
2.730 Å(57)
2.600 Å(90)
2.564 Å(40)
2.400 Å(42)
2.101 Å(42)
2.076 Å(42)
2.028 Å(42)
Comments:
Ōmi, Niigata Prefecture, Japan. The data are from Komatsu et al. (1973).

Geological EnvironmentHide

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

Type Occurrence of OhmiliteHide

General Appearance of Type Material:
Aggregates of very fine-grained crystals or occasionally spherulitic aggregates of radially arranged crystals in interstitial parts of albite aggregates. To 0.2 mm.
Place of Conservation of Type Material:
Niigata University, Niigata, Japan (type).
Geological Setting of Type Material:
In an amphibole-quartz-albitite dike cutting serpentinite.
Associated Minerals at Type Locality:
Reference:
Mizota, T., Komatsu, M., Chihara, K. (1973) On the crystal structure of Sr3TiSi4O12(OH).2H2O, a new mineral. Mineralogical Journal Japan: 7(3): 302-305.

Synonyms of OhmiliteHide

Other Language Names for OhmiliteHide

German:Ohmilit
Japanese:青海石
Russian:Омилит
Spanish:Ohmilita

Common AssociatesHide

Associated Minerals Based on Photo Data:
1 photo of Ohmilite associated with Magnesio-riebeckite◻{Na2}{Mg3Fe3+2}(Si8O22)(OH)2
1 photo of Ohmilite associated with AlbiteNa(AlSi3O8)

Related Minerals - Strunz-mindat GroupingHide

9.DH.Gageite-2M(Mn,Mg,Zn)42Si16O54(OH)40Mon. 2/m
9.DH.BavsiiteBa2V2O2[Si4O12]Tet. 4/m : I4/m
9.DH.DevilliersiteCa4Ca2Fe3+10O4[(Fe3+10Si2)O36]Tric. 1 : P1
9.DH.YuzuxiangiteSr3Fe3+(Si2O6)2(OH) · 3H2OMon. 2/m : P21/m
9.DH.LouisfuchsiteCa2(Mg4Ti2)(Al4Si2)O20Tric. 1 : P1
9.DH.05LeucophaniteNaCaBeSi2O6FOrth. 2 2 2 : P21 21 21
9.DH.15HaradaiteSrVSi2O7Orth. mmm (2/m 2/m 2/m)
9.DH.15SuzukiiteBaVSi2O7Orth.
9.DH.20BatisiteBaNaNaTi2(Si4O12)O2Orth. mmm (2/m 2/m 2/m) : Imma
9.DH.20Shcherbakovite(K,Ba)KNa(Ti,Nb)2(Si4O12)O2Orth. mmm (2/m 2/m 2/m) : Imma
9.DH.20NoonkanbahiteBaKNaTi2(Si4O12)O2Orth. mmm (2/m 2/m 2/m) : Imma
9.DH.25TaikaniteSr3BaMn2+2(Si4O12)O2Mon. 2 : B2
9.DH.30KrauskopfiteBaSi2O5 · 3H2OMon. 2/m : P21/b
9.DH.35Balangeroite(Mg,Fe2+,Fe3+,Mn2+)42Si16O54(OH)40Mon. 2/m
9.DH.35GageiteMn21(Si4O12)2O3(OH)20Mon. 2/m
9.DH.40AenigmatiteNa4[Fe2+10Ti2]O4[Si12O36]Tric. 1 : P1
9.DH.40DorriteCa4(Mg3Fe3+9)O4(Si3Al8Fe3+O36)Tric.
9.DH.40HøgtuvaiteCa4[Fe2+6Fe3+6]O4[Si8Be2Al2O36]Tric. 1 : P1
9.DH.40KrinoviteNa2Mg4Cr3+2(Si6O18)O2Tric. 1 : P1
9.DH.40Makarochkinite(Ca,Na)4[Fe2+8Fe3+2Ti2]O4[Si8Be2Al2O36]Tric. 1 : P1
9.DH.40RhöniteCa4[Mg8Fe3+2Ti2]O4[Si6Al6O36]Tric. 1 : P1
9.DH.40SerendibiteCa4[Mg6Al6]O4[Si6B3Al3O36]Tric. 1 : P1
9.DH.40WelshiteCa4Mg9Sb3O4[Si6Be3AlFe2O36]Tric. 1 : P1
9.DH.40WilkinsoniteNa2Fe2+4Fe3+2(Si6O18)O2Tric. 1 : P1
9.DH.40LeucorhöniteCa2(Mg,Fe3+,Al)6(Si,Al)6O20Tric.
9.DH.40KuratiteCa2(Fe2+5Ti)O2[Si4Al2O18]Tric. 1 : P1
9.DH.40KhesiniteCa4(Mg3Fe3+9)O4(Fe3+9Si3)O36Tric. 1 : P1
9.DH.40UM1991-29-SiO:FeMgNaNa4(Mg5Fe3+7)O4[Si9Fe3+3O36]
9.DH.45SapphirineMg4(Mg3Al9)O4[Si3Al9O36]Mon. 2/m : P21/b
9.DH.50Khmaralite(Mg,Al,Fe)16[(Al,Si,Be)12O36]O4Mon. 2/m : P21/b
9.DH.55Surinamite(Mg,Fe)3Al4BeSi3O16Mon. 2/m
9.DH.55UM1988-26-SiO:AlMgMg4Al2O[Si3Al2O15]
9.DH.60Deerite(Fe,Mn)6(Fe,Al)3[Si6O17]O3(OH)5Mon. 2/m : P21/b
9.DH.65HowieiteNa(Fe,Mn)10(Fe,Al)2Si12O31(OH)13Tric.
9.DH.65Taneyamalite(Na,Ca)(Mn,Mg,Fe)12Si12(O,OH)44Tric.
9.DH.70JohninnesiteNa2Mn2+9Mg7(OH)8[AsO4]2[Si6O17]2Tric.
9.DH.75AgrelliteNaCa2Si4O10FTric. 1 : P1

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 OhmiliteHide

References for OhmiliteHide

Localities for OhmiliteHide

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.
Japan
 
  • Niigata Prefecture
... +1 other reference
Komatsu et al. (1973)
        • Hashidate
Hiroaki Tano specimen +1 other reference
Hiroaki Tano's collection
 
矿物 and/or 产地  
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