Vote for your favorite mineral in #MinCup26! - Azurite vs. Smithsonite
It's carbonate-vs-carbonate to kick off Mineral Cup 2026 with copper-rich Azurite against zinc-rich Smithsonite.
Log InRegister
Quick Links : The Mindat ManualThe Rock H. Currier Digital LibraryMindat Newsletter [Free Download]
Home PageAbout MindatThe Mindat ManualHistory of MindatCopyright StatusWho We AreContact UsAdvertise on Mindat
Donate to MindatCorporate SponsorshipSponsor a PageSponsored PagesMindat AdvertisersAdvertise on Mindat
Learning CenterWhat is a mineral?The most common minerals on earthInformation for EducatorsMindat ArticlesThe ElementsThe Rock H. Currier Digital LibraryGeologic TimeExplore Fossils
Minerals by PropertiesMinerals by ChemistryMineral Visual ExplorerAdvanced Locality SearchRandom MineralRandom LocalitySearch by minIDLocalities Near MeSearch ArticlesSearch GlossaryMore Search Options
Search For:
Mineral Name:
Locality Name:
Keyword(s):
 
The Mindat ManualAdd a New PhotoRate PhotosLocality Edit ReportCoordinate Completion ReportAdd Glossary Item
Mining CompaniesStatisticsUsersMineral MuseumsClubs & OrganizationsMineral Shows & EventsThe Mindat DirectoryDevice SettingsThe Mineral QuizTime Machine
Photo SearchPhoto GalleriesSearch by ColorPhoto Colour ExplorerNew Photos TodayNew Photos YesterdayMembers' Photo GalleriesPast Photo of the Day GalleryPhotography

Reinerite

A valid IMA mineral species - grandfathered
This page is currently not sponsored. Click here to sponsor this page.
Hide all sections | Show all sections

About ReineriteHide

Formula:
Zn3(AsO3)2
Colour:
Originally blue toyellow green; also colorless to white
Lustre:
Adamantine, Vitreous
Hardness:
5 - 5½
Specific Gravity:
4.270
Crystal System:
Orthorhombic
Name:
Named in 1958 by Bruno H. Geier and K. Weber in honor of Willy Reiner [1895–1965], Senior Chemist, Tsumeb Corporation, Tsumeb, Namibia, who analyzed the type material.
A synthetic polymorph has been reported by Harrison (2010).


Unique IdentifiersHide

Mindat ID:
3386
Long-form identifier:
mindat:1:1:3386:8

Similar NamesHide

GreineriteA variety of DolomiteCaMg(CO3)2
RenieriteA valid IMA mineral species - grandfathered(Cu+,Zn)11Fe4(Ge4+,As5+)2S16

IMA Classification of ReineriteHide

Approved, 'Grandfathered' (first described prior to 1959)
IMA Formula:
Zn2+3(As3+O3)2
First published:
1958

Classification of ReineriteHide

4.JA.10

4 : OXIDES (Hydroxides, V[5,6] vanadates, arsenites, antimonites, bismuthites, sulfites, selenites, tellurites, iodates)
J : Arsenites, antimonites, bismuthites, sulfites, selenites, tellurites; iodates
A : Arsenites, antimonites, bismuthites; without additional anions, without H2O
45.1.1.1

45 : ACID AND NORMAL ANTIMONITES AND ARSENITES
1 : Miscellaneous

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

Physical Properties of ReineriteHide

Adamantine, Vitreous
Comment:
Vitreous to adamantine on fracture surfaces.
Colour:
Originally blue toyellow green; also colorless to white
Comment:
Light yellow-green, changing to sea-blue on exposure.
Hardness:
5 - 5½ on Mohs scale
Cleavage:
Distinct/Good
{110}, {011}, {111}, good
Density:
4.270 g/cm3 (Measured)    4.283 g/cm3 (Calculated)

Optical Data of ReineriteHide

Type:
Biaxial (-)
RI values:
nα = 1.749 nβ = 1.790 nγ = 1.821
Max. Birefringence:
δ = 0.072
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. Each grain retains its interference colour (retardation) while its brightness falls to black at extinction and reaches a maximum between extinction positions.

Surface Relief:
Very High (positive)
Relative to Canada balsam mounting medium (n ≈ 1.537).

This shows the grain boundary and Becke line effect under plane-polarised light, based on the contrast between this mineral's average refractive index and the mounting medium. It does not take into account mineral colouration.
In focus
Interference Figure:
This shows the idealized biaxial acute bisectrix (Bxa) interference figure - the conoscopic view for a grain cut perpendicular to the acute bisectrix, using this mineral's 2V. The two small white dots mark the melatopes - the points where the two optic axes emerge - and are shown only when they fall within the field of view. The coloured bands are isochromatics, and the dark bands are isogyres.

Rotate the stage: at 0°/90° the isogyres form a cross through the melatopes; at 45° they pull apart into curved hyperbolas. That splitting on rotation - absent in a uniaxial figure - is the standard diagnostic test for telling biaxial minerals from uniaxial ones. If 2V is large, the melatopes may fall outside the field of view, as they often do at the microscope too.

No measured or calculated 2V is on file for this mineral, so the value used here (80°) is estimated from its recorded refractive indices and optic sign, not from a direct 2V measurement.
Dispersion:
r > v moderate

Chemistry of ReineriteHide

Mindat Formula:
Zn3(AsO3)2
Element Weights:
Element% weight
Zn44.378 %
As33.903 %
O21.720 %

Calculated from ideal end-member formula.
Zn
As
O

Crystallography of ReineriteHide

Crystal System:
Orthorhombic
Class (H-M):
mmm(2/m2/m2/m) - Dipyramidal
Space Group:
Pbam
Setting:
Pbam
Cell Parameters:
a = 6.0883(2) Å, b = 14.3941(5) Å, c = 7.8022(2) Å
Ratio:
a:b:c = 0.423 : 1 : 0.542
Unit Cell V:
683.75 ų (Calculated from Unit Cell)
Z:
4

Crystal StructureHide

Load
Unit Cell | Unit Cell Packed
2x2x2 | 3x3x3 | 4x4x4
Show
Big Balls | Small Balls | Just Balls | Spacefill
Polyhedra Off | Si Polyhedra | All Polyhedra
Remove metal-metal sticks
Display Options
Black Background | White Background
Perspective On | Perspective Off
2D | Stereo | Red-Blue | Red-Cyan
View
CIF File    Best | x | y | z | a | b | c
Rotation
Stop | Start
Labels
Console Off | On | Grey | Yellow
IDSpeciesReferenceLinkYearLocalityPressure (GPa)Temp (K)
0000602ReineriteGhose S, Boving P, LaChapelle W A, Wan C (1977) Reinerite, Zn3(AsO3)2: an arsenite with a novel type of Zn-tetrahedral double chain American Mineralogist 62 1129-113419770293
CIF Raw Data - click here to close

X-Ray Powder DiffractionHide

Powder Diffraction Data:
d-spacingIntensity
3.9954 Å(1000)
2.6455 Å(290)
1.5488 Å(191)
3.2025 Å(187)
2.7826 Å(176)
2.6023 Å(145)
3.3942 Å(143)

Geological EnvironmentHide

Paragenetic Mode(s):
Paragenetic ModeEarliest Age (Ga)
Stage 7: Great Oxidation Event<2.4
47a : [Near-surface hydration of prior minerals]
47d : [Arsenates, antimonates, selenates, bismuthinates]
Stage 10b: Anthropogenic minerals<10 Ka
56 : Slag and smelter minerals (see also #51 and #55)

Type Occurrence of ReineriteHide

General Appearance of Type Material:
Crystals are rough, pseudohexagonal.
Place of Conservation of Type Material:
ENSM, Paris, France, number 50963.
IMK-TU, Berlin, Germany, 94/32, 86/70, 86/71.
Associated Minerals at Type Locality:

Other Language Names for ReineriteHide

Dutch:Reineriet
German:Reinerit
Simplified Chinese:砷锌矿
Spanish:Reinerita

Common AssociatesHide

Associations Based on Photo Data:
6 photos of Reinerite associated with LegranditeZn2(AsO4)(OH) · H2O
4 photos of Reinerite associated with GermaniteCu13Fe2Ge2S16
1 photo of Reinerite associated with Tennantite SubgroupCu6(Cu4C2+2)As4S12S
1 photo of Reinerite associated with AdamiteZn2(AsO4)(OH)
1 photo of Reinerite associated with LeiteiteZn(As2O4)
1 photo of Reinerite associated with GalliteCuGaS2
1 photo of Reinerite associated with SmithsoniteZnCO3
1 photo of Reinerite associated with ChalcociteCu2S
1 photo of Reinerite associated with SchaurteiteCa3Ge(SO4)2(OH)6 · 4H2O
1 photo of Reinerite associated with LudlockitePbFe3+4As3+10O22

Related Minerals - Strunz-mindat GroupingHide

4.JA.05LeiteiteZn(As2O4)Mon. 2/m : P21/b
4.JA.15KaribibiteFe3+3(As3+O2)4(As3+2O5)(OH)Orth. mmm(2/m2/m2/m) : Pnma
4.JA.20ManganoschafarzikiteMnSb2O4Tet. 4/mmm(4/m2/m2/m) : P42/mbc
4.JA.20TrippkeiteCu2+As3+2O4Tet. 4/mmm(4/m2/m2/m) : P42/mbc
4.JA.20SchafarzikiteFe2+Sb3+2O4Tet. 4/mmm(4/m2/m2/m) : P42/mbc
4.JA.20KusachiiteCuBi2O4Tet. 4/mmm(4/m2/m2/m) : P4/nnc
4.JA.20IgelströmiteFe3+(Sb3+Pb2+)O4Tet. 4/mmm(4/m2/m2/m) : P42/mbc
4.JA.25ApuaniteFe2+Fe3+4Sb3+4O12STet. 4/mmm(4/m2/m2/m) : P42/mbc
4.JA.30VersiliaiteFe2Fe4Sb6O16SOrth. mmm(2/m2/m2/m) : Pbam
4.JA.35SchneiderhöhniteFe2+Fe3+3As3+5O13Tric. 1 : P1
4.JA.40Zimbabweite(Na,K)2PbAs4(Ta,Nb,Ti)4O18Orth. mmm(2/m2/m2/m)
4.JA.45LudlockitePbFe3+4As3+10O22Tric. 1 : P1
4.JA.50PaulmooreitePb2[As2O5]Mon. 2/m : P21/b
4.JA.55StibivaniteSb2VO5Orth.
4.JA.60Chadwickite(UO2)[HAsO3]Tet.

Fluorescence of ReineriteHide

Fluoresces medium olive-green

Other InformationHide

Special Storage/
Display Requirements:
Light yellow-green, changing to sea-blue on exposure.
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 ReineriteHide

References for ReineriteHide

Reference List:

Localities for ReineriteHide

Showing 5 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.
Hide all sections | Show all sections

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.
China
 
  • Tibet
    • Qamdo Prefecture (Changdu Prefecture)
      • Riwoqê Co. (Leiwuqi Co.)
Yingchao Liu et al. (2013)
Germany
 
  • Lower Saxony
    • Goslar District
      • Langelsheim
        • Grane Reservoir
Schnorrer-Köhler (1991)
Namibia (TL)
 
  • Oshikoto Region
    • Tsumeb
Geier +1 other reference
Russia
 
  • Krasnoyarsk Krai
    • Western Sayan range
Kiseleva et al. (2024)
USA
 
  • New Jersey
    • Sussex County
      • Ogdensburg
        • Sterling Hill
Bostwick et al. (2017) +1 other reference
 
and/or  
Mindat.org® is an outreach project of the Hudson Institute of Mineralogy, a 501(c)(3) not-for-profit organization. Mindat® and mindat.org® are registered trademarks of the Hudson Institute of Mineralogy.
Copyright © mindat.org and the Hudson Institute of Mineralogy 1993-2026, except where stated. Most political location boundaries are © OpenStreetMap contributors. Mindat.org relies on the contributions of thousands of members and supporters. Founded in 2000 by Jolyon Ralph and Ida Chau.
Content on this site may not be used to train, fine-tune, or otherwise develop artificial intelligence or machine learning models without prior written permission - see our Terms & Conditions.
To cite: Ralph, J., Von Bargen, D., Martynov, P., Zhang, J., Que, X., Prabhu, A., Morrison, S. M., Li, W., Chen, W., & Ma, X. (2025). Mindat.org: The open access mineralogy database to accelerate data-intensive geoscience research. American Mineralogist, 110(6), 833–844. doi:10.2138/am-2024-9486.
Privacy Policy - Terms & Conditions - Contact Us / DMCA issues - Report a bug/vulnerability Current server date and time: September 1, 2026 19:40:23 Page updated: August 25, 2026 09:30:15
Go to top of page