Ishiharaite
A valid IMA mineral species
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Formula:
(Cu,Ga,Fe,In,Zn)S
Colour:
Dark gray
Lustre:
Metallic
Crystal System:
Isometric
Member of:
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.
Unique Identifiers
Mindat ID:
46067
Long-form identifier:
mindat:1:1:46067:9
GUID
(UUID V4):
(UUID V4):
64d7fae0-28f8-4dbc-893c-d7378ffe16da
IMA Classification of Ishiharaite
Approved
Approval year:
2013
First published:
2014
Classification of Ishiharaite
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.
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 Symbols
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.
Please only use the official IMA–CNMNC symbol. Older variants are listed for historical use only.
Symbol | Source | Reference |
---|---|---|
Ish | IMA–CNMNC | Warr, L.N. (2021). IMA–CNMNC approved mineral symbols. Mineralogical Magazine, 85(3), 291-320. doi:10.1180/mgm.2021.43 |
Ish | The 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 Ishiharaite
Optical Data of Ishiharaite
Reflectivity:
Wavelength | R1 | R2 |
---|---|---|
470nm | 6.77% | 18.27% |
546nm | 7.91% | 20.10% |
589nm | 8.96% | 21.74% |
650nm | 10.44% | 23.94% |
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 Ishiharaite
Mindat Formula:
(Cu,Ga,Fe,In,Zn)S
Crystallography of Ishiharaite
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 Structure
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Data courtesy of the American Mineralogist Crystal Structure Database. Click on an AMCSD ID to view structure
ID | Species | Reference | Link | Year | Locality | Pressure (GPa) | Temp (K) |
---|---|---|---|---|---|---|---|
0020262 | Ishiharaite | Marquez-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 52 969-980 | 2015 | Capillitas mine, Argentina | 0 | 293 |
CIF Raw Data - click here to close
X-Ray Powder Diffraction
Powder Diffraction Data:
d-spacing | Intensity |
---|---|
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 Environment
Paragenetic Mode(s):
Paragenetic Mode | Earliest Age (Ga) |
---|---|
High-𝑇 alteration and/or metamorphism | |
33 : Minerals deposited by hydrothermal metal-rich fluids (see also [#12]) |
Type Occurrence of Ishiharaite
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 Ishiharaite
Relationship of Ishiharaite to other Species
Member of:
Other Members of this group:
Browneite | MnS | Iso. 4 3m : F4 3m |
Coloradoite | HgTe | Iso. 4 3m : F4 3m |
Hawleyite | CdS | Iso. 4 3m : F4 3m |
Metacinnabar | HgS | Iso. 4 3m : F4 3m |
Rudashevskyite | (Fe,Zn)S | Iso. 4 3m : F4 3m |
Sphalerite | ZnS | Iso. 4 3m : F4 3m |
Stilleite | ZnSe | Iso. 4 3m : F4 3m |
Tiemannite | HgSe | Iso. 4 3m : F4 3m |
Related Minerals - Strunz-mindat Grouping
2.CB. | Agmantinite | Ag2MnSnS4 |
2.CB. | Richardsite | Zn2CuGaS4 |
2.CB. | Gachingite | Au(Te1-xSex) |
2.CB. | Tolstykhite | Au3S4Te6 |
2.CB. | Hanswilkeite | KFeS2 |
2.CB. | Auroselenide | AuSe |
2.CB. | Ruizhongite | (Ag2◻)Pb3Ge2S8 |
2.CB. | Okruginite | Cu2SnSe3 |
2.CB.05a | Coloradoite | HgTe |
2.CB.05a | Hawleyite | CdS |
2.CB.05a | Metacinnabar | HgS |
2.CB.05c | Polhemusite | (Zn,Hg)S |
2.CB.05b | Sakuraiite | (Cu,Zn,Fe)3(In,Sn)S4 |
2.CB.05a | Sphalerite | ZnS |
2.CB.05a | Stilleite | ZnSe |
2.CB.05a | Tiemannite | HgSe |
2.CB.05 | UM1998-15-S:CuFeZn | Cu2Fe3Zn5S10 |
2.CB.05a | Rudashevskyite | (Fe,Zn)S |
2.CB.07a | Shenzhuangite | NiFeS2 |
2.CB.07a | Unnamed (Cu-Mn-Sn Sulpide) | Cu2MnSnS4 |
2.CB.10a | Chalcopyrite | CuFeS2 |
2.CB.10a | Eskebornite | CuFeSe2 |
2.CB.10a | Gallite | CuGaS2 |
2.CB.10b | Haycockite | Cu4Fe5S8 |
2.CB.10a | Lenaite | AgFeS2 |
2.CB.10b | Mooihoekite | Cu9Fe9S16 |
2.CB.10b | Putoranite | Cu1.1Fe1.2S2 |
2.CB.10a | Roquesite | CuInS2 |
2.CB.10b | Talnakhite | Cu9(Fe,Ni)8S16 |
2.CB.10a | Laforêtite | AgInS2 |
2.CB.10a | Unnamed (Cu-Zn-In Sulphide) | CuZn2InS4 |
2.CB.10a | UM1984-30-S:CuFeSn | Cu2Fe2Sn3S7 |
2.CB.10c | Omariniite | Cu8Fe2ZnGe2S12 |
2.CB.15a | Černýite | Cu2(Cd,Zn,Fe)SnS4 |
2.CB.15a | Ferrokësterite | Cu2FeSnS4 |
2.CB.15a | Hocartite | Ag2(Fe2+,Zn)SnS4 |
2.CB.15a | Idaite | Cu5FeS6 |
2.CB.15a | Kësterite | Cu2ZnSnS4 |
2.CB.15a | Kuramite | Cu3SnS4 |
2.CB.15b | Mohite | Cu2SnS3 |
2.CB.15a | Pirquitasite | Ag2ZnSnS4 |
2.CB.15a | Stannite | Cu2FeSnS4 |
2.CB.15c | Stannoidite | Cu+6Cu2+2(Fe2+,Zn)3Sn2S12 |
2.CB.15a | Velikite | Cu2HgSnS4 |
2.CB.15c | UM2006-11-S:CuFeGeZn | Cu8(Fe,Zn)3Ge2S12 (?) |
2.CB.17a v | Arsenic-bearing Renierite | Cu11GeAsFe4S16 |
2.CB.20 | Chatkalite | Cu6FeSn2S8 |
2.CB.20 | Mawsonite | Cu6Fe2SnS8 |
2.CB.30 | Argyropyrite | near Ag2Fe7S11 |
2.CB.30 | Colusite | Cu13VAs3S16 |
2.CB.30 | Germanite | Cu13Fe2Ge2S16 |
2.CB.30 | Germanocolusite | Cu26V2(Ge,As)6S32 |
2.CB.30 | Nekrasovite | Cu26V2(Sn,As,Sb)6S32 |
2.CB.30 | Stibiocolusite | Cu13V(Sb,Sn,As)3S16 |
2.CB.30 | Ovamboite | Cu20(Fe,Cu,Zn)6W2Ge6S32 |
2.CB.30 | Maikainite | Cu20(Fe,Cu)6Mo2Ge6S32 |
2.CB.30 | Frieseite | Ag2Fe5S8 (?) |
2.CB.35a | Hemusite | Cu6SnMoS8 |
2.CB.35a | Kiddcreekite | Cu6SnWS8 |
2.CB.35a | Polkovicite | (Fe,Pb)3(Ge,Fe)1-xS4 |
2.CB.35a | Renierite | (Cu1+,Zn)11Fe4(Ge4+,As5+)2S16 |
2.CB.35a | Vinciennite | Cu+7Cu2+3Fe2+2Fe3+2Sn(As,Sb)S16 |
2.CB.35a | Morozeviczite | (Pb,Fe)3Ge1-xS4 |
2.CB.35b | Catamarcaite | Cu6GeWS8 |
2.CB.40 | Lautite | CuAsS |
2.CB.42 | Lingbaoite | AgTe3 |
2.CB.45 | Cadmoselite | CdSe |
2.CB.45 | Greenockite | CdS |
2.CB.45 | Wurtzite | (Zn,Fe)S |
2.CB.45 | Rambergite | MnS |
2.CB.45 | Buseckite | (Fe,Zn,Mn)S |
2.CB.45 | Maletoyvayamite | Au3Se4Te6 |
2.CB.47 | Murchisite | Cr5S6 |
2.CB.50 | Zincselenide | ZnSe |
2.CB.50 | Wassonite | TiS |
2.CB.52 | Dzhezkazganite | ReMoCu2PbS6 ? |
2.CB.55a | Cubanite | CuFe2S3 |
2.CB.55b | Isocubanite | CuFe2S3 |
2.CB.60 | Picotpaulite | TlFe2S3 |
2.CB.60 | Raguinite | TlFeS2 |
2.CB.65 | Argentopyrite | AgFe2S3 |
2.CB.65 | Sternbergite | AgFe2S3 |
2.CB.70 | Sulvanite | Cu3VS4 |
2.CB.75 | Vulcanite | CuTe |
2.CB.80 | Empressite | AgTe |
2.CB.85 | Muthmannite | AuAgTe2 |
Other Information
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 Ishiharaite
mindat.org URL:
https://www.mindat.org/min-46067.html
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References for Ishiharaite
Localities for Ishiharaite
Locality List
- 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.
All localities listed without proper references should be considered as questionable.
Argentina (TL) | |
| Williams et al. (2014) +2 other references |
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