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Kintoreite

A valid IMA mineral species
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About KintoreiteHide

Formula:
PbFe3(PO4)(PO3OH)(OH)6
Colour:
Cream to yellowish green and brownish yellow.
Lustre:
Vitreous, Greasy
Hardness:
4
Specific Gravity:
4.34 (Calculated)
Crystal System:
Trigonal
Name:
After the type locality, the Kintore opencut, Broken Hill, Yancowinna Co., New South Wales, Australia.
The phosphate analogue of segnitite. Forms a solid-solution series with corkite and segnitite (Kintoreite-Segnitite Series).

Related to kolitschite.



Unique IdentifiersHide

Mindat ID:
2214
Long-form identifier:
mindat:1:1:2214:5

Similar NamesHide

KantoriteA valid IMA mineral speciesK2NaMg(SO4)2F
Kintoreite-2cPbFe33+(PO4)2(OH,H2O)6
KondöriteA synonym of Konderite

IMA Classification of KintoreiteHide

Classification of KintoreiteHide

8.BL.10

8 : PHOSPHATES, ARSENATES, VANADATES
B : Phosphates, etc., with additional anions, without H2O
L : With medium-sized and large cations, (OH, etc.):RO4 = 3:1
42.7.3.6

42 : HYDRATED PHOSPHATES, ETC.CONTAINING HYDROXYL OR HALOGEN
7 : (AB)2(XO4)Zq·xH2O

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

Physical Properties of KintoreiteHide

Vitreous, Greasy
Transparency:
Transparent
Colour:
Cream to yellowish green and brownish yellow.
Streak:
Pale yellowish green
Hardness:
Tenacity:
Brittle
Cleavage:
Distinct/Good
On {001}
Density:
4.34 g/cm3 (Calculated)

Optical Data of KintoreiteHide

Type:
Uniaxial (-)
RI values:
nω = 1.935 - 1.955 nε = 1.935
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 uniaxial interference figure - the conoscopic (convergent-light, Bertrand-lens-in) view, for a grain cut with the optic axis centred and vertical. The coloured rings are isochromatics, computed with the same physics as the Michel-Lévy bar above; the dark cross is the isogyre.

For a genuinely uniaxial mineral viewed this way, that cross stays perfectly stationary if you rotate the stage - unlike a biaxial mineral, where it splits apart on rotation. That invariance is itself the standard diagnostic test for telling uniaxial and biaxial minerals apart at the microscope.
Pleochroism:
Visible
Comments:
Light yellowish green to medium yellow.

Chemistry of KintoreiteHide

Mindat Formula:
PbFe3(PO4)(PO3OH)(OH)6
Element Weights:
Element% weight
O33.545 %
Pb31.031 %
Fe25.090 %
P9.277 %
H1.057 %

Calculated from ideal end-member formula.
O
Pb
Fe
P
H

Crystallography of KintoreiteHide

Crystal System:
Trigonal
Class (H-M):
3m(32/m) - Hexagonal Scalenohedral
Space Group:
R3m
Cell Parameters:
a = 7.2963(5) Å, c = 16.8491(5) Å
Ratio:
a:c = 1 : 2.309
Unit Cell V:
776.81 ų (Calculated from Unit Cell)
Z:
3
Comment:
Date for near endmember composition (Grey et al., 2009)

Crystal StructureHide

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IDSpeciesReferenceLinkYearLocalityPressure (GPa)Temp (K)
0004932KintoreiteGrey I E, Mumme W G, Mills S J, Birch W D, Wilson N C (2009) The crystal chemical role of Zn in alunite-type minerals: Structure refinements for kintoreite and zincian kintoreite American Mineralogist 94 676-6832009Kintore mine at Broken Hill, New South Wales0293
0004931KintoreiteGrey I E, Mumme W G, Mills S J, Birch W D, Wilson N C (2009) The crystal chemical role of Zn in alunite-type minerals: Structure refinements for kintoreite and zincian kintoreite American Mineralogist 94 676-6832009Schone Aussicht mine, near Dernbach, Germany0293
0014525KintoreiteKharisun, Taylor M R, Bevan D J M, Pring A (1997) The crystal structure of kintoreite, PbFe3(PO4)2(OH,H2O)6 Mineralogical Magazine 61 123-1291997Kintore opencut, Broken Hill, New South Wales, Australia0293
CIF Raw Data - click here to close

X-Ray Powder DiffractionHide

Powder Diffraction Data:
d-spacingIntensity
3.07 Å(100)
5.96 Å(90)
3.67 Å(60)
2.538 Å(50)
2.257 Å(50)
1.979 Å(50)
2.971 Å(40)

Geological EnvironmentHide

Paragenetic Mode(s):

Type Occurrence of KintoreiteHide

General Appearance of Type Material:
Clusters and coatings of cream to yellowish green rhombohedral crystals up to 2 mm. It also forms waxy, yellowish green globular crusts and hemispheres on other phosphate minerals.
Place of Conservation of Type Material:
The South Australia Museum, Adelaide, Australia, G14354
Museum Victoria, Melbourne, Australia, M42891.
Geological Setting of Type Material:
Oxidation of primary ore rich in galena, in the presence of solutions with high P/(As + S) ratios.
Associated Minerals at Type Locality: