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Junitoite

A valid IMA mineral species
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About JunitoiteHide

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Jun Ito
Formula:
CaZn2Si2O7 · H2O
Colour:
Colorless
Lustre:
Adamantine, Vitreous, Sub-Vitreous
Hardness:
Specific Gravity:
3.5
Crystal System:
Orthorhombic
Name:
Named by Sidney Arthur Williams in 1976 in honor of Jun Ito (25 September 1926, Japan - 6 June 1978, Chicago, Illinois, USA), mineralogist and crystallographer, University of Chicago, Chicago, IL, USA. He first noted the compound, in 1968, in a series of experiments of synthesis of Pb-Ca-Zn silicates.
This page provides mineralogical data about Junitoite.


Unique IdentifiersHide

Mindat ID:
2123
Long-form identifier:
mindat:1:1:2123:0

Similar NamesHide

JuanitaiteA valid IMA mineral species(Cu,Ca,Fe)10Bi(AsO4)4(OH)11 · 2H2O
JuaniteA valid IMA mineral species - grandfathered - questionableCa10Mg4Al2Si11O39 · 4H2O or near
JungiteA valid IMA mineral speciesCa2Zn4Fe83+(PO4)9(OH)9 · 16H2O
JunoiteA valid IMA mineral speciesCu2Pb3Bi8(S,Se)16
JuonniiteA valid IMA mineral speciesCaMgSc(PO4)2(OH) · 4H2O

IMA Classification of JunitoiteHide

Approved
IMA Formula:
CaZn2+2Si2O7·H2O
Approval year:
1975
First published:
1976

Classification of JunitoiteHide

9.BD.15

9 : SILICATES (Germanates)
B : Sorosilicates
D : Si2O7 groups, with additional anions; cations in tetrahedral [4] and greater coordination
56.2.1.1

56 : SOROSILICATES Si2O7 Groups, With Additional O, OH, F and H2O
2 : Si2O7 Groups and O, OH, F, and H2O with cations in [4] and/or >[4] coordination
14.7.17

14 : Silicates not Containing Aluminum
7 : Silicates of Ba, Sr and Zn

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

Physical Properties of JunitoiteHide

Adamantine, Vitreous, Sub-Vitreous
Transparency:
Transparent
Colour:
Colorless
Comment:
Sometimes milky white to pale lavender due to alteration.
Streak:
White
Hardness:
4½ on Mohs scale
Tenacity:
Very brittle
Cleavage:
Very Good
{010} very good,{100} and {101} are poor.
Fracture:
Micaceous
Comment:
Breaks somewhat like mica in that the plates separate easily by breaking using a sharp point.
Density:
3.5 g/cm3 (Measured)    3.506 g/cm3 (Calculated)
Comment:
Dcalc from Yang et al. (2012)

Optical Data of JunitoiteHide

Type:
Biaxial (+)
RI values:
nα = 1.656 nβ = 1.664 nγ = 1.672
2V:
Measured: 86° , Calculated: 88°
Birefringence:
0.016
Max. Birefringence:
δ = 0.016
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.
Dispersion:
r < v, very weak
Optical Extinction:
X = b; Y = a; Z = c.
Pleochroism:
Non-pleochroic

Chemistry of JunitoiteHide

Mindat Formula:
CaZn2Si2O7 · H2O
Element Weights:
Element% weight
Zn36.625 %
O35.851 %
Si15.733 %
Ca11.226 %
H0.565 %

Calculated from ideal end-member formula.
Zn
O
Si
Ca
H

Crystallography of JunitoiteHide

Crystal System:
Orthorhombic
Class (H-M):
mm2 - Pyramidal
Space Group:
Aba2
Cell Parameters:
a = 12.51 Å, b = 6.31 Å, c = 8.56 Å
Ratio:
a:b:c = 1.983 : 1 : 1.357
Unit Cell V:
675.71 ų (Calculated from Unit Cell)
Z:
4
Morphology:
Crystals to 5mm with hemimorphic development. c {001}, b {010}, k {101}, p {111}, r {131}, -r {131}, -g {191}. (Viscinal forms may show herringbone pattern ["whishbone"]).
Comment:
Cell re-set from original

Crystal StructureHide

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IDSpeciesReferenceLinkYearLocalityPressure (GPa)Temp (K)
0019356JunitoiteYang H, Jenkins N G, Downs R T (2012) Redetermination of junitoite, CaZn2Si2O7*H2O Acta Crystallographica E68 i73-i732012Christmas Mine, Gila County, Arizona, USA0293
0014480JunitoiteHamilton R D, Finney J J (1985) The structure of junitoite, CaZn2Si2O7*H2O Mineralogical Magazine 49 91-951985Christmas mine, Gile County, Arizona, USA0293
CIF Raw Data - click here to close

X-Ray Powder DiffractionHide

Powder Diffraction Data:
d-spacingIntensity
6.25 Å(40)
4.70 Å(50)
3.53 Å(100)
2.82 Å(100)
2.54 Å(100)
2.52 Å(50)
2.35 Å(70)
1.540 Å(60)
Comments:
ICDD 29-394

Geological EnvironmentHide

Paragenetic Mode(s):
Paragenetic ModeEarliest Age (Ga)
High-? alteration and/or metamorphism
32 : Ba/Mn/Pb/Zn deposits, including metamorphic deposits
Stage 7: Great Oxidation Event<2.4
47a : [Near-surface hydration of prior minerals]

Type Occurrence of JunitoiteHide

General Appearance of Type Material:
Randomly oriented colorless to lavender platy crystals up to 5 x 0.5 mm.
Place of Conservation of Type Material:
University of Arizona, Tucson, Arizona, USA.
Harvard University, Cambridge, Massachusetts, USA, 119097.
National Museum of Natural History, Washington, D.C., USA, 136688.
University of Paris, Paris, France.
National School of Mines, Paris, France.
The Natural History Museum, London, England, 1980,535.
Geological Setting of Type Material:
Contact metamorphosed zinc orebody.
Associated Minerals at Type Locality:

Synonyms of JunitoiteHide

Other Language Names for JunitoiteHide

Common AssociatesHide

Associations Based on Photo Data:
7 photos of Junitoite associated with KinoiteCa2Cu2(H2O)2[Si3O10]
4 photos of Junitoite associated with DioptaseCuSiO3 · H2O
3 photos of Junitoite associated with Smectite GroupA0.3D2-3[T4O10]Z2 · nH2O
2 photos of Junitoite associated with ChalcanthiteCuSO4 · 5H2O
2 photos of Junitoite associated with GilaliteCu5Si6O17 · 7H2O
1 photo of Junitoite associated with Hydroxyapophyllite-(K)KCa4(Si8O20)(OH,F) · 8H2O
1 photo of Junitoite associated with RuiziteCa2Mn3+2[Si4O11(OH)2](OH)2 · 2H2O
1 photo of Junitoite associated with SauconiteNa0.3Zn3((Si,Al)4O10)(OH)2 · 4H2O

Related Minerals - Strunz-mindat GroupingHide

9.BD.05BertranditeBe4(Si2O7)(OH)2Orth. mm2 : Cmc21
9.BD.10HemimorphiteZn4Si2O7(OH)2 · H2OOrth. mm2 : Imm2
9.BD.20TinzeniteCa2Mn2+4Al4[B2Si8O30](OH)2Tric. 1 : P1
9.BD.20Axinite-(Fe)Ca2Fe2+Al2BSi4O15OHTric. 1 : P1
9.BD.20DubińskaiteCa4Sc2Al4[Be2Si8O30](OH)2Tric. 1 : P1
9.BD.20Axinite-(Mg)Ca2MgAl2BSi4O15OHTric. 1 : P1
9.BD.20Axinite-(Mn)Ca2Mn2+Al2BSi4O15(OH)Tric. 1 : P1
9.BD.25VistepiteSnMn4B2Si4O16(OH)2Tric. 1 : P1
9.BD.30BoralsiliteAl16B6O30(Si2O7)Mon. 2/m : B2/m
9.BD.35Werdingite(Mg,Fe)2Al14Si4B4O37Tric. 1 : P1
9.BD.40VránaiteAl16B4Si4O38Mon. 2/m : B2/m

Fluorescence of JunitoiteHide

Not fluorescent.

Other InformationHide

Thermal Behaviour:
Strongly pyroelectric.
Notes:
Easily soluble in cold 10% HCl or 1:7 HNO3, but is insoluble in water. Slowly decomposed by hot 40% KOH.

Heated in a closed tube, it quickly turns milky-white, spalling into flakes that separate on {010}. Water is lost during the process, and it fuses to a clear glassy bead.
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 JunitoiteHide

References for JunitoiteHide

Localities for JunitoiteHide

Showing 4 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.
Sri Lanka
 
  • North Central Province
    • Anuradhapura District
Chandrakumara et al. (2021)
USA (TL)
 
  • Arizona
    • Gila County
      • Banner Mining District
        • Christmas
Williams (1976) +1 other reference
Williams (1976) +1 other reference
  • New Jersey
    • Sussex County
      • Franklin
Dunn (1995)
 
and/or  
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