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Paratooite-(La)

A valid IMA mineral species
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About Paratooite-(La)Hide

Formula:
(La,Sr,Ca)4CuCa(Na,Ca)2(CO3)8
Colour:
Pale turquoise-blue to pale blue
Lustre:
Vitreous, Pearly
Hardness:
4
Specific Gravity:
3.68
Crystal System:
Orthorhombic
Name:
For the type locality, the Paratoo copper mine, Australia. The suffix/modifier follows the IMA Levinson rule for minerals with essential REE, and denotes predominant lanthanum.
Unique combination of elements. In terms of atomic arrangement, paratooite-(La) is a 1 x 2 x 2 superstructure of carbocernaite. The mineral also shows an interesting carbonate-nitrate diadochy, as shown below.


Unique IdentifiersHide

Mindat ID:
27579
Long-form identifier:
mindat:1:1:27579:8

Similar NamesHide

PeretaiteA valid IMA mineral speciesCa(SbO)4(SO4)2(OH)2 · 2H2O

IMA Classification of Paratooite-(La)Hide

Classification of Paratooite-(La)Hide

5.AD.20

5 : CARBONATES (NITRATES)
A : Carbonates without additional anions, without H2O
D : With rare-earth elements (REE)

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

Physical Properties of Paratooite-(La)Hide

Vitreous, Pearly
Transparency:
Transparent
Colour:
Pale turquoise-blue to pale blue
Streak:
Pale blue
Hardness:
Comment:
Hardness estimated based on other REE carbonates. Aggregate hardness was 2.
Cleavage:
None Observed
TEM studies indicate a cleavage parallel to {100}
Density:
3.68(3) g/cm3 (Measured)    3.78 g/cm3 (Calculated)
Comment:
Measured using the suspension method, with Clerici solution diluted with water

Optical Data of Paratooite-(La)Hide

Type:
Biaxial (-)
RI values:
nα = 1.605(3) nβ = 1.696(3) nγ = 1.752(2)
2V:
Calculated: 72.6°
Max. Birefringence:
δ = 0.147
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.
Pleochroism:
Visible
Comments:
Medium strong; X = very pale bluish; Y = Z = bluish (with greenish tint).
Comments:
Absorption: Z ≈ Y >> X.

Chemistry of Paratooite-(La)Hide

Mindat Formula:
(La,Sr,Ca)4CuCa(Na,Ca)2(CO3)8
Element Weights:
Element% weight
La46.876 %
O32.396 %
C8.107 %
Cu5.361 %
Na3.879 %
Ca3.381 %

Calculated from ideal end-member formula.
La
O
C
Cu
Na
Ca

Crystallography of Paratooite-(La)Hide

Crystal System:
Orthorhombic
Class (H-M):
mmm(2/m2/m2/m) - Dipyramidal
Space Group:
Pbam
Cell Parameters:
a = 7.2250(3) Å, b = 12.7626(5) Å, c = 10.0559(4) Å
Ratio:
a:b:c = 0.566 : 1 : 0.788
Unit Cell V:
927.25 ų
Comment:
Data from Krivovichev et al. (2019). Wallwork et al. (2006) gives the following unit-cell parameters, determined from synchrotron powder diffraction data (indexed on a primitive orthorhombic cell): a = 10.0862(5), b = 12.8088(6), c = 7.2360(4) Å, V = 934.8(1) Å3; they could not determine the crystal structure, but suggested several possible space groups.

X-Ray Powder DiffractionHide

Geological EnvironmentHide

Paragenetic Mode(s):
Paragenetic ModeEarliest Age (Ga)
Near-surface Processes
23 : Subaerial aqueous alteration by non-redox-sensitive fluids (see also #47)

Type Occurrence of Paratooite-(La)Hide

General Appearance of Type Material:
Sheaves and radiating sprays of blade-like to tabular pale blue crystals in thin fissures in a slaty country rock. Individual crystals are typically 50-200 µm in maximum dimension but <5 µm thick.
Place of Conservation of Type Material:
South Australian Museum, Adelaide (G29614).
Geological Setting of Type Material:
Copper and REE deposit

From type description: Formation took place under conditions of intense weathering in an arid climate, probably at neutral or slightly basic pH and oxidizing conditions, with evaporation of saline groundwaters playing an important role.
Associated Minerals at Type Locality:

Synonyms of Paratooite-(La)Hide

Other Language Names for Paratooite-(La)Hide

Simplified Chinese:帕碳铜镧石
Traditional Chinese:帕碳銅鑭石

Common AssociatesHide

Associations Based on Photo Data:
8 photos of Paratooite-(La) associated with Kamphaugite-(Y)Ca(Y,REE)(CO3)2(OH) · H2O
4 photos of Paratooite-(La) associated with MalachiteCu2(CO3)(OH)2
3 photos of Paratooite-(La) associated with Bastnäsite-(La)La(CO3)F

Related Minerals - Strunz-mindat GroupingHide

5.AD.05Sahamalite-(Ce)(Mg,Fe)(Ce,La,Nd)2(CO3)4Mon. 2/m : P21/c
5.AD.15Rémondite-(La)Na3(La,Ca,Na)3(CO3)5Mon. 2 : P21
5.AD.15Rémondite-(Ce)Na3(Ce,Ca,Na)3(CO3)5Mon. 2 : P21
5.AD.15Petersenite-(Ce)Na4(Ce,La,Nd)2(CO3)5Mon. 2 : P21

Fluorescence of Paratooite-(La)Hide

No visible fluorescence

Other InformationHide

Notes:
Quickly reacts with with effervescence in dilute HCl. Dissolves slowly in cold 10% HNO3, but reacts rapidly, with effervescence and discolouration, when the solution is heated.
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 Paratooite-(La)Hide

References for Paratooite-(La)Hide

Localities for Paratooite-(La)Hide

Showing 1 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.
Australia (TL)
 
  • South Australia
    • District Council of Peterborough
      • Paratoo
Pring et al. (2006) +2 other references
 
and/or  
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