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Ishiharaite

A valid IMA mineral species
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02632970017055636589921.jpg
Photo of Shunzo Ishihara
Formula:
(Cu,Ga,Fe,In,Zn)S
Colour:
Dark gray
Lustre:
Metallic
Crystal System:
Isometric
Name:
Named in honour of Dr. Shunso Ishihara (石原舜三), a leading authority on the links between the genesis of granitic rocks and mineralization. Dr. Shunso Ishihara was born on March 10, 1934 in the town of Fuchu, 6 km east of Hiroshima, Japan. On the morning of August 6, 1945, he witnessed the bombing and destruction of Hiroshima by American forces, and that afternoon, attended to the burned and injured who fled the city. He attended the University of Hiroshima, and obtained his B.Sc. degree in geology in 1956. The same year, he joined the Geological Survey of Japan (GSJ), at a time when the Japanese government had committed itself to investigate the peaceful uses of nuclear energy. Thus began his focus on the genesis of molybdenite deposits of Japan, commonly associated with uraninite. He tackled a study of the Questa Mo deposits in New Mexico for his M.Sc. thesis, defended at Columbia University in New York (1963). In his D.Sc. thesis (University of Tokyo, 1970), he concluded that calc-alkaline granitic rocks, such as occur in the Japanese island arc, vary in their inherent degree of oxidation according to their geographic location. Belts of magnetite-series (oxidized) and ilmenite-series (reduced) granites were found to differ in their pattern of mineralization. The magnetite–ilmenite scheme remains the basis of metallogenic classification of granites to this day. In 1985, Dr. Ishihara became the head of the Mineral Resources Department of the GSJ, and in 1989, its Director. He retired in 1997. He has published widely on the geochemical and mineralogical attributes of oxidized and reduced granites in Japan and abroad. Among the many awards given to him are the Silver Medal of the Society of Economic Geology (1989) and the Gold Medal of the Society for Geology Applied to Mineral Deposits (2009). He passed away in 2020. He was also Emeritus Advisor of AIST (Advanced Industrial Science and Technology), Tsukuba, Japan. He made relationships between the degree of oxidation of a granite magma and the ore mineralization.
Sphalerite structure type.

Compare also sakuraiite.


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Unique IdentifiersHide

Mindat ID:
46067
Long-form identifier:
mindat:1:1:46067:9
GUID
(UUID V4):
64d7fae0-28f8-4dbc-893c-d7378ffe16da

IMA Classification of IshiharaiteHide

Classification of IshiharaiteHide

2.CB.05a

2 : SULFIDES and SULFOSALTS (sulfides, selenides, tellurides; arsenides, antimonides, bismuthides; sulfarsenites, sulfantimonites, sulfbismuthites, etc.)
C : Metal Sulfides, M: S = 1: 1 (and similar)
B : With Zn, Fe, Cu, Ag, etc.

Mineral SymbolsHide

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

Please only use the official IMA–CNMNC symbol. Older variants are listed for historical use only.

SymbolSourceReference
IshIMA–CNMNCWarr, L.N. (2021). IMA–CNMNC approved mineral symbols. Mineralogical Magazine, 85(3), 291-320. doi:10.1180/mgm.2021.43
IshThe Canadian Mineralogist (2019)The Canadian Mineralogist (2019) The Canadian Mineralogist list of symbols for rock- and ore-forming minerals (December 30, 2019). download

Physical Properties of IshiharaiteHide

Metallic
Transparency:
Opaque
Colour:
Dark gray
Comment:
Greater than tennantite

Optical Data of IshiharaiteHide

Reflectivity:
WavelengthR1R2
470nm6.77%18.27%
546nm7.91%20.10%
589nm8.96%21.74%
650nm10.44%23.94%

Reflectance graph
Graph shows reflectance levels at different wavelengths (in nm). Top of box is 100%. Peak reflectance is 23.94%.
R1 shown in black, R2 shown in red
Colour in reflected light:
burgundy brown with a faint violet hue in air and violet-burgundy in oil.

Chemistry of IshiharaiteHide

Mindat Formula:
(Cu,Ga,Fe,In,Zn)S

Crystallography of IshiharaiteHide

Crystal System:
Isometric
Class (H-M):
4 3m - Hextetrahedral
Space Group:
F4 3m
Setting:
F4 3m
Cell Parameters:
a = 5.368(1) Å
Unit Cell V:
154.68 ų
Z:
4
Morphology:
As subhedral, equidimensional, individual grains.

Crystal StructureHide

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IDSpeciesReferenceLinkYearLocalityPressure (GPa)Temp (K)
0020262IshiharaiteMarquez-Zavalia M F, Galliski M A, Drabek M, Vymazalova A, Watanabe Y, Murakami H, Bernhardt H J (2015) Ishiharaite, (Cu,Ga,Fe,In,Zn)S, a new mineral from the Capillitas mine, Northwestern Argentina The Canadian Mineralogist 52 969-9802015Capillitas mine, Argentina0293
CIF Raw Data - click here to close

X-Ray Powder DiffractionHide

Powder Diffraction Data:
d-spacingIntensity
3.096 Å(100)
2.684 Å(20)
1.898 Å(60)
1.620 Å(40)
1.344 Å(10)
1.231 Å(10)
1.097 Å(15)
1.035 Å(10)
Comments:
From Type Description.

Geological EnvironmentHide

Paragenetic Mode(s):
Paragenetic ModeEarliest Age (Ga)
High-𝑇 alteration and/or metamorphism
33 : Minerals deposited by hydrothermal metal-rich fluids (see also [#12])

Type Occurrence of IshiharaiteHide

General Appearance of Type Material:
As subhedral, equidimensional, individual grains (20 to 50 μm in size) included in tennantite
Place of Conservation of Type Material:
Type material is deposited in the collections of the Museo de Mineralogiá ‘‘Alfred Stelzner’’, Universidad Nacional de Córdoba, Córdoba, Argentina, catalogue number 3280
Geological Setting of Type Material:
Epithermal ore deposit
Associated Minerals at Type Locality:
Reference:
Márquez-Zavalía, M.F., Galliski, M.Á., Drábek, M., Vymazalová, A., Watanabe, Y., Murakami, H., Bernhardt, H.-J. (2014) Ishiharaite, (Cu,Ga,Fe,In,Zn)S, a new mineral from the Capillitas Mine, Northwestern Argentina. Canadian Mineralogist: 52: 969-980.

Synonyms of IshiharaiteHide

Relationship of Ishiharaite to other SpeciesHide

Other Members of this group:
BrowneiteMnS Iso. 4 3m : F4 3m
ColoradoiteHgTeIso. 4 3m : F4 3m
HawleyiteCdSIso. 4 3m : F4 3m
MetacinnabarHgSIso. 4 3m : F4 3m
Rudashevskyite(Fe,Zn)SIso. 4 3m : F4 3m
SphaleriteZnSIso. 4 3m : F4 3m
StilleiteZnSeIso. 4 3m : F4 3m
TiemanniteHgSeIso. 4 3m : F4 3m

Related Minerals - Strunz-mindat GroupingHide

2.CB.AgmantiniteAg2MnSnS4Orth.
2.CB.RichardsiteZn2CuGaS4Tet. 4 2m : I4 2m
2.CB.GachingiteAu(Te1-xSex)Orth. mmm (2/m 2/m 2/m)
2.CB.TolstykhiteAu3S4Te6Tric. 1 : P1
2.CB.HanswilkeiteKFeS2Mon. 2/m : B2/b
2.CB.AuroselenideAuSeMon. 2/m : B2/m
2.CB.Ruizhongite(Ag2◻)Pb3Ge2S8Iso. 4 3m : I4 3d
2.CB.OkruginiteCu2SnSe3Mon. m : Bb
2.CB.05aColoradoiteHgTeIso. 4 3m : F4 3m
2.CB.05aHawleyiteCdSIso. 4 3m : F4 3m
2.CB.05aMetacinnabarHgSIso. 4 3m : F4 3m
2.CB.05cPolhemusite(Zn,Hg)STet.
2.CB.05bSakuraiite(Cu,Zn,Fe)3(In,Sn)S4 Iso.
2.CB.05aSphaleriteZnSIso. 4 3m : F4 3m
2.CB.05aStilleiteZnSeIso. 4 3m : F4 3m
2.CB.05aTiemanniteHgSeIso. 4 3m : F4 3m
2.CB.05UM1998-15-S:CuFeZnCu2Fe3Zn5S10
2.CB.05aRudashevskyite(Fe,Zn)SIso. 4 3m : F4 3m
2.CB.07aShenzhuangiteNiFeS2Tet. 4 2m : I4 2d
2.CB.07aUnnamed (Cu-Mn-Sn Sulpide)Cu2MnSnS4
2.CB.10aChalcopyriteCuFeS2Tet. 4 2m : I4 2d
2.CB.10aEskeborniteCuFeSe2Tet. 4 2m : P4 2c
2.CB.10aGalliteCuGaS2Tet. 4 2m : I4 2d
2.CB.10bHaycockiteCu4Fe5S8Orth. 2 2 2
2.CB.10aLenaiteAgFeS2Tet. 4 2m : I4 2d
2.CB.10bMooihoekiteCu9Fe9S16Tet. 4 2m : P4 2m
2.CB.10bPutoraniteCu1.1Fe1.2S2Iso. m3m (4/m 3 2/m) : Pn3m
2.CB.10aRoquesiteCuInS2Tet. 4 2m : I4 2d
2.CB.10bTalnakhiteCu9(Fe,Ni)8S16Iso. 4 3m : I4 3m
2.CB.10aLaforêtiteAgInS2Tet. 4 2m : I4 2d
2.CB.10aUnnamed (Cu-Zn-In Sulphide)CuZn2InS4
2.CB.10aUM1984-30-S:CuFeSnCu2Fe2Sn3S7
2.CB.10cOmariniiteCu8Fe2ZnGe2S12Orth. 2 2 2 : I2 2 2
2.CB.15aČernýiteCu2(Cd,Zn,Fe)SnS4Tet. 4 2m : I4 2m
2.CB.15aFerrokësteriteCu2FeSnS4Tet. 4 : I4
2.CB.15aHocartiteAg2(Fe2+,Zn)SnS4Tet. 4 2m : I4 2m
2.CB.15aIdaiteCu5FeS6Hex.
2.CB.15aKësteriteCu2ZnSnS4Tet. 4 : I4
2.CB.15aKuramiteCu3SnS4Tet. 4 2m : I4 2m
2.CB.15bMohiteCu2SnS3Mon.
2.CB.15aPirquitasiteAg2ZnSnS4Tet. 4 : I4
2.CB.15aStanniteCu2FeSnS4Tet. 4 2m : I4 2m
2.CB.15cStannoiditeCu+6Cu2+2(Fe2+,Zn)3Sn2S12Orth. 2 2 2 : I2 2 2
2.CB.15aVelikiteCu2HgSnS4Tet. 4 : I4
2.CB.15cUM2006-11-S:CuFeGeZnCu8(Fe,Zn)3Ge2S12 (?)
2.CB.17a vArsenic-bearing RenieriteCu11GeAsFe4S16
2.CB.20ChatkaliteCu6FeSn2S8Tet. 4 2m : P4m2
2.CB.20MawsoniteCu6Fe2SnS8Tet. 4 2m : P4m2
2.CB.30Argyropyritenear Ag2Fe7S11
2.CB.30ColusiteCu13VAs3S16Iso. 4 3m : P4 3n
2.CB.30GermaniteCu13Fe2Ge2S16Iso. 4 3m : P4 3n
2.CB.30GermanocolusiteCu26V2(Ge,As)6S32Iso. 4 3m : P4 3m
2.CB.30NekrasoviteCu26V2(Sn,As,Sb)6S32Iso. 4 3m : P4 3n
2.CB.30StibiocolusiteCu13V(Sb,Sn,As)3S16Iso. 4 3m : P4 3m
2.CB.30Ovamboite Cu20(Fe,Cu,Zn)6W2Ge6S32Iso. 4 3m : P4 3n
2.CB.30MaikainiteCu20(Fe,Cu)6Mo2Ge6S32Iso. m3m (4/m 3 2/m)
2.CB.30FrieseiteAg2Fe5S8 (?)
2.CB.35aHemusiteCu6SnMoS8Iso.
2.CB.35aKiddcreekiteCu6SnWS8Iso. 4 3m : F4 3m
2.CB.35aPolkovicite(Fe,Pb)3(Ge,Fe)1-xS4Iso.
2.CB.35aRenierite(Cu1+,Zn)11Fe4(Ge4+,As5+)2S16Tet. 4 2m : P4 2c
2.CB.35aVincienniteCu+7Cu2+3Fe2+2Fe3+2Sn(As,Sb)S16Tet.
2.CB.35aMorozeviczite(Pb,Fe)3Ge1-xS4Iso.
2.CB.35bCatamarcaiteCu6GeWS8Hex. 6mm : P63mc
2.CB.40LautiteCuAsSOrth. mmm (2/m 2/m 2/m) : Pnma
2.CB.42LingbaoiteAgTe3Trig. 3m : R3m
2.CB.45CadmoseliteCdSeHex. 6mm : P63mc
2.CB.45GreenockiteCdSHex. 6mm : P63mc
2.CB.45Wurtzite(Zn,Fe)SHex. 6mm : P63mc
2.CB.45RambergiteMnSHex. 6mm : P63mc
2.CB.45Buseckite(Fe,Zn,Mn)SHex. 6mm : P63mc
2.CB.45MaletoyvayamiteAu3Se4Te6Tric. 1 : P1
2.CB.47MurchisiteCr5S6Trig. 3m (3 2/m) : P3 1c
2.CB.50ZincselenideZnSe
2.CB.50WassoniteTiSTrig. 3m (3 2/m) : R3m
2.CB.52DzhezkazganiteReMoCu2PbS6 ?Trig. 3m : R3m
2.CB.55aCubaniteCuFe2S3Orth. mmm (2/m 2/m 2/m)
2.CB.55bIsocubaniteCuFe2S3Iso. m3m (4/m 3 2/m) : Fm3m
2.CB.60PicotpauliteTlFe2S3Orth. mmm (2/m 2/m 2/m) : Cmcm
2.CB.60RaguiniteTlFeS2Orth.
2.CB.65ArgentopyriteAgFe2S3Mon. 2/m
2.CB.65SternbergiteAgFe2S3Orth. mmm (2/m 2/m 2/m)
2.CB.70SulvaniteCu3VS4Iso. 4 3m : P4 3m
2.CB.75VulcaniteCuTeOrth. mmm (2/m 2/m 2/m)
2.CB.80EmpressiteAgTeOrth. mmm (2/m 2/m 2/m)
2.CB.85MuthmanniteAuAgTe2Mon. 2/m : P2/m

Other InformationHide

IR Spectrum:
Non-fluorescent.
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 IshiharaiteHide

References for IshiharaiteHide

Localities for IshiharaiteHide

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.
Argentina (TL)
 
  • Catamarca Province
    • Andalgalá Department
      • Capillitas mining district
Williams et al. (2014) +2 other references
 
and/or  
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