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Percleveite-(La)

A valid IMA mineral species
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Formula:
La2Si2O7
Colour:
Very pale yellow to colourless in thin fragments to light yellow in aggregates
Lustre:
Greasy
Hardness:
6
Specific Gravity:
5.094 (Calculated)
Crystal System:
Tetragonal
Name:
For being the La-dominant analogue of percleveite-(Ce).

In honour of Per Teodor Cleve (10 February 1840, Stockholm, Sweden - 18 June 1905, Uppsala, Sweden) - Swedish chemist, biologist, mineralogist, and oceanographer. He is best known for his discovery of the chemical elements holmium and thulium. Cleve earned his BSc and PhD from Uppsala University in 1863 and 1868, respectively. After receiving his PhD, he became an assistant professor of chemistry at the university. He later became professor of general and agricultural chemistry. In 1874, he theorised that didymium was in fact two elements; this theory was confirmed in 1885 when Carl Auer von Welsbach discovered neodymium and praseodymium.

In 1879 Cleve discovered holmium and thulium. His other contributions to chemistry include the discovery of aminonaphthalenesulfonic acids, also known as Cleve's acids. From 1890 on he focused on biological studies. He developed a method of determining the age and order of late glacial and postglacial deposits from the types of diatom fossils in the deposits, and wrote a seminal text in the field of oceanography.
The La-dominant analogue of percleveite-(Ce).


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Unique IdentifiersHide

Mindat ID:
53754
Long-form identifier:
mindat:1:1:53754:6

Similar NamesHide

Percleveite-(Ce)A valid IMA mineral speciesCe2Si2O7

IMA Classification of Percleveite-(La)Hide

Classification of Percleveite-(La)Hide

9.BC.35

9 : SILICATES (Germanates)
B : Sorosilicates
C : Si2O7 groups, without non-tetrahedral anions; cations in octahedral [6] and greater coordination

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
Pcv-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 Percleveite-(La)Hide

Greasy
Transparency:
Transparent
Colour:
Very pale yellow to colourless in thin fragments to light yellow in aggregates
Streak:
White
Hardness:
Hardness Data:
Measured
Comment:
Based on scratch tests
Tenacity:
Brittle
Cleavage:
Imperfect/Fair
Imperfect {001}
Fracture:
Irregular/Uneven
Density:
5.094 g/cm3 (Calculated)
Comment:
Calculated from the empirical formula

Optical Data of Percleveite-(La)Hide

Type:
Uniaxial (+)
RI values:
nω = 1.825(10) nε = 1.835(10)
Max. Birefringence:
δ = 0.010
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:
Moderate
Pleochroism:
Non-pleochroic

Chemistry of Percleveite-(La)Hide

Mindat Formula:
La2Si2O7
Element Weights:
Element% weight
La62.293 %
O25.112 %
Si12.595 %

Calculated from ideal end-member formula.

Crystallography of Percleveite-(La)Hide

Crystal System:
Tetragonal
Class (H-M):
4 - Pyramidal
Space Group:
P41
Cell Parameters:
a = 6.8482(3) Å, c = 24.8550(13) Å
Ratio:
a:c = 1 : 3.629
Unit Cell V:
1165.64 ų
Z:
8

X-Ray Powder DiffractionHide

Geological EnvironmentHide

Paragenetic Mode(s):
Paragenetic ModeEarliest Age (Ga)
Stage 4b: Highly evolved igneous rocks>3.0
37 : Layered igneous intrusions and related PGE minerals

Type Occurrence of Percleveite-(La)Hide

Synonyms of Percleveite-(La)Hide

Other Language Names for Percleveite-(La)Hide

Related Minerals - Strunz-mindat GroupingHide

9.BC.Anorthoyttrialite-(Y)Y4(SiO4)(Si3O10)Tric. 1 : P1
9.BC.KozłowskiiteCa4(Fe2+Sn3)[Si2O7]2[Si2O6OH]2Tric. 1
9.BC.05Yttrialite-(Y)(Y,Th)2Si2O7Mon. 2/m : P21/m
9.BC.05ThortveititeSc2Si2O7Mon. 2/m : B2/m
9.BC.05Keiviite-(Y)Y2Si2O7Mon. 2/m : B2/m
9.BC.05Keiviite-(Yb)Yb2Si2O7Mon. 2/m : B2/m
9.BC.05GittinsiteCaZrSi2O7Mon. 2 : B2
9.BC.10ParakeldyshiteNa2ZrSi2O7Tric. 1 : P1
9.BC.10Keldyshite(Na,H)2ZrSi2O7Tric. 1 : P1
9.BC.10KhibinskiteK2ZrSi2O7Mon. 2/m : B2/m
9.BC.10BrunovskyiteNaZrSi2O6(OH) Tric. 1 : P1
9.BC.15RankiniteCa3Si2O7Mon. 2/m : P21/b
9.BC.20BarysilitePb8Mn2+[Si2O7]3Trig. 3m(32/m) : R3c
9.BC.25Edgarbaileyite[Hg2]2+3[Si2O7]Mon.
9.BC.30KristianseniteCa4(Sc2Sn2)[Si2O7]2[Si2O6OH]2Tric. 1
9.BC.30NybergiteCa4Sc3Sn(Si2O7)(Si2O6OH)3Tric. 1 : P1
9.BC.30SilesiaiteCa4(Fe3+2Sn2)[Si2O7]2[Si2O6OH]2Tric. 1
9.BC.35Percleveite-(Ce)Ce2Si2O7Tet. 4 : P41
9.BC.40ScottyiteBaCu2Si2O7Orth. mmm(2/m2/m2/m) : Pmna

Fluorescence of Percleveite-(La)Hide

Does not fluoresce under ultraviolet light.

Other InformationHide

Notes:
Does not react with either cold hydrochloric or nitric acids.
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 Percleveite-(La)Hide

References for Percleveite-(La)Hide

Localities for Percleveite-(La)Hide

Showing 2 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.
Austria
 
  • Salzburg
    • Zell am See District
      • Kaprun
Kolitsch et al. (2021)
Russia (TL)
 
  • Chelyabinsk Oblast
    • Kyshtym
Miyawaki et al. (2019) +2 other references
 
and/or  
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